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Report on the 2018 Diamond Drilling Program

North Abitibi Property, Cochrane District, Ontario

Larder Lake Mining Division

Hoblitzell Township, Ontario

UTM NAD 83 (Zone 17) 577300 mE, 5482000 mN

NTS 32E05 & 32E12

FOR

125 Don Hillock Dr., Unit 18

Aurora, Ontario

L4G 0H8

Monique Ruhl, BSc

Rob McEwan, BSc

March 7, 2019

i

TABLE OF CONTENTS

INTRODUCTION AND PROPERTY DESCRIPTION.................................................................. 1

REGIONAL AND PROPERTY GEOLOGY ................................................................................. 4

HISTORIC EXPLORATION ACTIVITIES ................................................................................... 8

EXPLORATION WORK CONDUCTED BY TRI ORIGIN ............................................................ 8

FALL 2018 DRILL PROGRAM ..................................................................................................10

Diamond drill hole NA18-01 ...................................................................................................12



Geochemical Summary Overview ..........................................................................................15

Drill Site Completion ..............................................................................................................18

CONCLUSIONS AND RECOMMENDATIONS ..........................................................................19

REFERENCES .........................................................................................................................20

PERSONNEL ............................................................................................................................21

STATEMENT OF QUALIFICATIONS ........................................................................................22

APPENDICES ...........................................................................................................................24

LIST OF FIGURES

Figure 1. North Abitibi Property Location. ................................................................................... 2

Figure 2. Mining claim tenure map. ............................................................................................ 3

Figure 3. Major mines in the northern Abitibi Subprovince. ........................................................ 6

Figure 4. Geological interpretation of the North Abitibi Property. ................................................ 7

LIST OF TABLES

Table 1 List of mining claims on which work was performed. ..................................................... 1

Table 2. Diamond drill hole locations and details (NAD 83/17). .................................................10

Table 3. Diamond drill hole survey details. ................................................................................11

Table 4. Significant geochemical results, sorted by hole ID then depth. ....................................17

ii

LIST OF APPENDICES

Appendix A: Assay Procedures

Appendix B: Drill Logs

Appendix C: Cross Sections

Appendix D: Geochemical Certificates of Analysis

Appendix E: Geochemical Results

LIST OF MAPS

Map 1. Diamond Drill Hole Geology Plan Map. Scale 1:10 000

1

INTRODUCTION AND PROPERTY DESCRIPTION

This report details the processes and results of the fall 2018 drilling program on the

North Abitibi Property, by Tri Origin Exploration Ltd. Three completed drill holes and two failed

attempts, totaling 1624 meters, were drilled between September 25 and October 29, 2018. Due

to complications with the sole access road from inclement fall weather, the program was ended

before all planned drilling was completed.

Tri Origin’s North Abitibi property is located in Hoblitzell Township, Larder Lake Mining

Division, approximately 20 km west of the Ontario/Québec border and 120 km northeast of

Cochrane, Ontario (figure 1). Vehicle access to the property is via the gravel Tomlinson Road,

which departs north from Trans-Limit Road at kilometer 89 as measured from Cochrane. The

property consists of 187 Single Cell Mining Claims and 28 Boundary Cell Mining Claims,

covering an area of approximately 50 square kilometers. The claims are held as to a 100%

interest by Tri Origin Exploration Ltd. and all claims are in good standing until at least January

27, 2020. The drilling program was conducted in the central portion of the property, west of

Spade Lake (figure 2). Cell claims on which drilling and associated work was performed on are

listed in Table 1 and shown in figure 2.

Table 1 List of mining claims on which work was performed.

Mining Claim Tenure No. Title Type Cell Due Date (yyyy/mm/dd)

193008 Single Cell Mining Claim 2020/01/27



2

Figure 1. North Abitibi Property Location.

3

Figure 2. Mining claim tenure map.

4

REGIONAL AND PROPERTY GEOLOGY

The North Abitibi Property is situated in the northwest corner of the Archean age Abitibi

Greenstone Belt. This portion of the greenstone belt hosts the Mattagami, Selbaie, Joutel and

Casa-Berardi mining camps in Quebec and the Detour Lake Mine in Ontario (figure 3). The

geology of the property is largely known from a synthesis of drill core logging, geophysical

interpretation, and overburden stripping near Tomlinson Road (figure 4). Outcrop exposure is

rare on the property, at <1%.

From most northerly extent of the property to the Spade Lake Zone, the property is

underlain by east-west striking primarily volcaniclastic and sedimentary rocks. Iron-rich

sediments as banded magnetite–silica–amphibole+/-garnet beds occur along the southern

contact of this assemblage, and the sediments are intruded by gabbro at the eastern part of the

property.

The Spade Lake Zone consists of mafic to felsic volcanic rocks with minor volcaniclastic

sediments, intruded by sills of the “Spade Lake Porphyry” which are most abundant at the south

part of the zone. The Spade Lake Porphyry is a coarse grained, porphyritic felsic intrusion with a

granodiorite to granite composition. Felsic tuffs predominate in the western part of this belt and

mafic volcanic flows and volcaniclastics are more common in the eastern part of this belt.

Historic drill logs and drill core samples indicate the presence of agglomeritic or conglomeritic

sedimentary units east along strike from the Spade Lake Zone. Structural information from drill

core suggests a moderate to steep northerly dip for most lithologies.

The area between the Spade Lake Zone and the Road Gold Zone is less well known,

primarily because most drill holes were stopped once they intersected the Spade Lake

Porphyry. This area consists of a mixed unit of intermediate volcanic rock interpreted to extend

the length of the property. It is likely intruded by a quartz feldspar porphyry, based on historic

drill logs.

Lying to the south of this belt is another mixed assemblage composed of felsic to mafic

volcanic flows and volcaniclastic rocks, which dip at 60 to 70° north. A large portion of this area

was exposed during 2011 and 2016 trenching conducted by Tri Origin. This area is referred to

as the Road Gold Zone. The northern edge of the trenched area is underlain by amphibole-rich

basalt and tuffaceous amphibolitic schist dipping moderately to steeply to the north. The mafic

volcanic rocks contain well foliated sections of intense iron carbonate alteration as bedding-

parallel layers and veinlets (with 5 to 10% vein density). Outcropping south of the mafic unit are

magnetite-rich dacitic to rhyodacitic volcanic, pyroclastic, and volcaniclastic rocks. Trenching

uncovered bomb-bearing, dacitic, pyroclastic flows and ash tuffs. Bombs are comprised of

feldspar-crystal tuffs, and are quite large and stretched, ranging from 0.5 to 5 m in length and up

to 1 m in width, with significant amounts of pyrite and chalcopyrite (up to 10%) locally

associated with quartz veins. A broad area of argillaceous sedimentary rock occurs south of this

volcanic assemblage along the southern margin of the property.

5

Gold mineralization has been intersected by drilling at both the Spade Lake and Road

Gold Zones. The main Spade Lake zone is a west striking, stratabound and, in places,

stratiform, altered felsic to intermediate tuff located near the north margin of Spade Lake. The

Road Gold zone is a west-striking zone of laminated, ash tuff located 1.3 km south of the Spade

Lake zone immediately west of the Tomlinson Road. A third gold mineralized zone occurs south

of Club Lake and may be associated with oxide-facies iron formation but has not been

evaluated by Tri Origin. Gold appears to be related to pyrite abundance and to a lesser extent,

silicification and quartz veins in altered felsic schists at Spade Lake. At the Road Gold Zone,

gold appears to be more abundant in pyritic tuff where there is a greater abundance of sulphidic

quartz veins and iron-carbonate alteration. Alteration accompanying the gold mineralization also

includes sericite, hematite, magnetite, chlorite and minor tourmaline.

6

Figure 3. Major mines in the northern Abitibi Subprovince.

7

Figure 4. Geological interpretation of the North Abitibi Property.

8

HISTORIC EXPLORATION ACTIVITIES

Due to the extensive overburden cover and lack of outcrop exposure, a variety of

airborne and ground geophysical survey programs (largely carried out by Cogema Canada Ltd.,

Newmont Exploration of Canada Ltd., and Esso Resources Canada Ltd.) have been the

principal methods of exploration on the property followed by reverse circulation (RC) and

diamond drilling. A total of 116 RC overburden holes and 96 diamond drill holes are spread over

the entire length of the property and the historical gold intercepts in diamond drilling represent

targets for future diamond drilling programs. The majority of the historic diamond drill holes on

the property were drilled by Cogema Canada Limited, Newmont Exploration of Canada Ltd., and

Tri Origin Exploration Ltd. The historic drill holes are further detailed by Learn, Mandziuk,

Perkins, and Harron (see references). Twenty-one of these holes reported at least one sample

> 2 grams Au per tonne over a 1 metre intersection.

The Road Gold zone was discovered during line cutting and bedrock mapping by

Newmont Exploration of Canada in the summer of 1985 (Archer, 1986). This discovery was

followed by a program of exploration between 1986 and 1987 which included an IP survey,

diamond drilling, RC overburden drilling, and overburden stripping.

EXPLORATION WORK CONDUCTED BY TRI ORIGIN

Tri Origin Exploration conducted diamond drilling in 2007 and 2008 (at both the Spade

Lake and Road zones), as well as overburden stripping in 2011 which expanded the surface

and subsurface extents of mineralization across 7 trenches at the Road Gold zone. The 2011

stripping program was cut short by the onset of winter. Geologic mapping of the trenches was

postponed and conducted in October 2014. Tri Origin geologists collected and assayed grab

samples from all of the trenches. Gold mineralization at the Road Gold zone was exposed at the

surface in trenches between 5,482,020 and 5,482,080 m N, and was recognized as striking

west to west-southwest and having a moderate to steep north dip. Assay results from drill core

have returned values up to 17.8 g/t Au, while grab samples from trenches have returned up to

43 g/t Au and 140 g/t Ag (Kendle 2012). In the fall of 2016 Tri Origin Exploration completed a

more extensive overburden stripping and rock sampling program in an attempt to expand the

known surface extension of the Road Gold zone. Overburden stripping was completed by

Digalot of Cochrane, ON. Twenty rock samples were collected from the new stripped area and

sent for assay (Au and Ag) and trace metals analysis (Cu, Zn, Pb, As, Ba, and Mo), as well as

ten outstanding rock samples from the 2011 exploration program. Eight overburden samples

were collected from the bedrock/overburden interface along the newly stripped walls and

analysed for gold plus base metals. Assay results from rock samples returned values of up to 20

g/t Au. Seven rock samples returned values greater than 500 ppb Au.

The 2016 overburden stripping program was conducted in conjunction with a line cutting

program and a 2D induced polarization (IP) survey. Line cutting was performed by A Star

Prospecting of Thunder Bay, ON, and IP surveying was performed by Dias Geophysical Ltd. of

Saskatoon, SK. In August 2018, prior to commencing diamond drilling, Tri Origin geologists

9

collected 23 grab samples from the Road Gold zone trenches which were sent for assay, as

well as trace element analyses. 9 were sent for major oxide analysis. Geochemical results are

summarized in a separate report filed with the Ontario government in 2019 (Ruhl and McEwan

2019). Assay results returned values of up to 7013 ppb Au. Three other samples returned Au

values above 1400 ppb. A more detailed geology map was produced of the main trench area

with refined geological contacts.

10

FALL 2018 DRILL PROGRAM

Between September 21st and November 8th, three diamond drill holes totaling 1388m

were completed within the North Abitibi property, one at the western Spade Lake zone and two

at the Road Gold zone. Two failed attempts occurred during the drilling of the holes at the Road

Gold zone. The drill was realigned and holes were re-drilled at adjusted azimuths. Drill core

from a hole drilled in 2007 by Tri Origin (NA-07-02) was obtained from the resident geology

office in Kirkland Lake and re-logged. Table 2 summarizes drill hole location details (coordinate

projection is in UTM NAD 83, zone 17) and table 3 lists survey results. Surveys were conducted

and recorded by Vital Drilling personnel using Reflex instrumentation. Azimuth was corrected for

a local declination of -10° west. All drilling operations were conducted by Vital Drilling from

Sudbury, ON. The drill was dragged from each site using a bull dozer and a tracked Muskeg.

Water saturated peat bogs hindered the progress of drill moves and made accessing drill sites

difficult. Core was brought to the Tomlinson road using ATVs or the dozer and transported to

Cochrane by a pick-up truck and trailer to be logged, photographed, cut, and sampled.

Samples were submitted to the SGS laboratory in Cochrane, ON, for fire assay and

measured by atomic absorption spectroscopy. Samples were then sent to SGS Lakefield, ON,

laboratory for multi-element analysis using multi-acid digestion and Inductively Coupled Plasma

Emission Mass Spectrometry. Laboratory procedures are appended in Appendix A. Analytical

results were compiled by Monique Ruhl and Rob McEwan of Tri Origin. Core from the program

was stacked and temporarily stored in Cochrane, ON. Drilling was supervised by Monique Ruhl

and Rob McEwan from Tri Origin Exploration Ltd.

Diamond drill hole logs are attached as Appendix B, drill sections are attach as Appendix

C, original geochemical certificates of analysis are attached as Appendix D, and geochemical

results are tabulated in Appendix E. Details and results of each drill hole are summarized and

presented below.

Table 2. Diamond drill hole locations and details (NAD 83/17).

Hole ID Collar Easting Collar Northing Elevation (m) Depth (m) Dip (°) Azimuth (°) Core size

NA18-01 576301 5482351 300 464 -72 170 NQ

NA18-02 576705 5482436 297 470 -64 170 NQ

NA18-03 576302 5483476 292 454 -65 170 NQ

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Table 3. Diamond drill hole survey details.

Hole ID Depth (m) Azimuth (°) Dip (°)

NA18-01 14 171.5 -71.6

NA18-01 50 172.3 -71.2

NA18-01 107 174.6 -70.2

NA18-01 143 175 -70.2

NA18-01 209 182.9 -69.3

NA18-01 173 181.8 -69.9

NA18-01 245 179.1 -69

NA18-01 302 185.7 -68

NA18-01 347 188.7 -67.2

NA18-01 419 192.2 -66

NA18-01 461 192 -64.5

NA18-01A 0 170 -70

NA18-01A 14 169.9 -70.6

NA18-01A 113 184.9 -55.8

NA18-01A 116 186 -55.5

NA18-02 29 173.9 -63.9

NA18-02 89 174.1 -62.5

NA18-02 116 174.3 -61.7

NA18-02 200 174 -60.8

NA18-02 302 178.2 -59.7

NA18-02 413 184.5 -56.5

NA18-02 470 185.2 -55.5

NA18-02A 0 168 -64

NA18-02A 29 176 -63.5

NA18-03 26 171.3 -64.6

NA18-03 101 174.2 -62.5

NA18-03 200 173.7 -61.5

NA18-03 302 177.4 -59.1

NA18-03 400 180.4 -59.1

NA18-03 454 178.6 -57.7

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DIAMOND DRILL HOLE NA18-01

NA18-01 was collared west of the main Road Gold zone trench. Drilling began

September 26th and was completed on October 4th. Preliminary logging was completed between

September 27th and October 10th by M Ruhl and R McEwan of Tri Origin Exploration Ltd. NA18-

01 was drilled for 464 meters. Water was pumped from the largest trench.

Target

NA18-01 was drilled to trace the extent and continuity of anomalous gold samples taken

from the Road Gold zone trench and anomalous drill core samples from historic Newmont drill

holes. These samples were taken close to the contact between mafic and felsic rocks. The

primary target was centered at 5482200 meters north on L3600 and at approximately 400m

depth. NA18-01 was collared north of the target.

Geology Log Summary

NA18-01 intersected bedrock at 5m in mafic metavolcanic rocks. The upper 331 meters

was a sequence of mafic metavolcanic rocks. This rock unit consisted of interbedded amphibole

metabasalts and tuffs. Contacts between flows and tuffs were gradual. The amphibole

metabasalt was a distinct unit characterized by medium grained green-black prismatic

amphibole phenocrysts in a fine to medium grained chloritic matrix. Tuffaceous units included

well foliated ash tuffs, a small section of lapilli tuff from 218 to 222 meters depth and a distinct

garnet-bearing tuff. The bottom of the mafic metavolcanic sequence, from 323 to 331, consisted

of iron-carbonate rich volcaniclastic rock also observed at surface in the trench. Sulphide

content of the rock was generally low, with only local sections of 1-3% disseminated py/po over

a maximum width of 6 meters and a few sulphide-bearing quartz-veins. Sulphide content

appeared to increase with depth. Foliation measurements from 5 to 174m depth were on

average 55° to the core axis (TCA). From 174 to 331m foliation measurements steepened to an

average of 64° TCA.

From 331 to 411.6m NA18-01 intersected a sequence of interbedded felsic banded tuffs

and a porphyritic crystal tuff with gradual contacts. The felsic tuff unit has previously been

described as ‘colour banded tuffs’. It is characterized by fine-grained, laminated, green and red

to pink bands. Compositional banding measurements were measured between 55-58° TCA.

Sericite and salmon-coloured alteration was observed between 339.5 and 367 meters depth.

The crystal tuff consists of light grey, 2mm, phenocrysts in a fine grained dark grey matrix.

The last 53m of the hole consisted of compositional banded intermediate volcanic flows.

There was a sharp contact between the overlying felsic tuffs to the intermediate volcanics. This

unit is characterized by alternating bands of light and dark grey fine grained material and is well-

foliated. Foliation measurements after 425 meters ranged from 44-47° TCA.

On average, 3-5% disseminated euhedral pyrite was observed between 339.5 and 347

meters depth in the colour banded tuff unit, with sections of up to 10%. This unit and

mineralization signature correlates along strike and dip with the targeted mafic-felsic boundary

described in historic drill logs. This target was hit sooner than expected, indicating that an

13

assume dip of 70° is likely too steep. The approximate dip of the contact between mafic and a

felsic unit is likely closer to 60°.

Assay samples from NA18-01 returned Au values below 1 ppb in the interbedded

amphibole metabasalts and tuffs. An increase in Au values was observed at the transition to

felsic banded tuff unit at approximately 339m depth. Most notably, sample 522039 returned a

Au value of 1.45 g/t from 343 and 344 meters. Samples 522035, 522036, and 522040 were also

taken from the colour banded tuff between 339.5 and 345 meters depth. They returned Au

values of 454, 274, and 216 ppb, over 1 meter intervals. Au values from 345 meters to the end

of the hole are low and comparable to the first 339 meters.


NA18-02 was collared north and east of the Road Gold zone trench. Drilling began

October 8th and was completed on October 19th. Preliminary logging was completed between

October 10th and October 21st by M Ruhl and R McEwan of Tri Origin Exploration Ltd. NA18-02

was drilled for 470 meters. Water was pumped from the west side of the Tomlinson Road, with

the water line crossing the road.

Target

NA18-02 was drilled to trace the extent and continuity of lithological contacts and the

high gold abundance near the stratigraphic footwall of the Road Gold zone indicated from

historic Newmont drill holes. Based on IP survey results, the primary target was centered at

5482200 meters north on L3700 and at approximately 350m depth. NA18-02 was collared to

intersect the footwall of the Road Gold zone at approximately 350 to 400m downhole, assuming

a 70° north dip.

Geology Log Summary

NA18-02 went through 19 meters of overburden, indicating an overburden depth of 17.1

meters, with a drill hole inclination of -64°. The upper 270 meters of the hole consists of mafic to

intermediate tuffs and volcaniclastic sediments, as well as flows. Mafic to intermediate tuffs

capped the first 39 meters after overburden. A massive crystal tuff unit with tightly packed

medium to coarse grained quartz and pale pink feldspar phenocrysts in finer grained black

matrix is interbedded with the mafic flows. The volcaniclastic sediments are characterized by

very fine grained alternating purple-brown and chlorite-rich beds. The sediments are

interbedded with finely laminated ash tuffs with minor garnet phenocrysts. Intermediate volcanic

flows consist of fine grained, pale grey compositionally banded flows. Banding was measured at

36° TCA. The amphibole metabasalt observed in NA18-01 was intersected between 110 to 140

and 205 to 260 meters in NA18-02. There was nil to trace sulphide mineralization within these

units. Foliation within these units was measured between 45 and 56° TCA.

From 270 meters to the end of the hole at 470 meters, the rock consisted of felsic

metavolcanic tuffs and flows. The northern part of this unit was characterized by the presence of

large lapilli fragments. From 270 to 293 meters the core consists of fine grained alternating light

grey/blue and pale green bands with subangular, elongated heterolithic clasts throughout.

Clasts range from <5mm to 70mm wide. There are minor cherty fragments throughout, as well

14

as clasts of massive sulphide from 313.8 to 323 meters depth. The lapilli tuff correlates to the

unit observed at surface in the Road Gold zone trenches. From 270 to 279.5 meters this unit

contained 3-5% disseminated py/po and 5% of sulphide along quartzo-feldspathic vein

boundaries. This mineralization correlates to that recorded in historic Newmount drill holes and

in NA-07-02 drilled by Tri Origin in 2007. This unit was intersected sooner in the core than

expected indicating a shallower dip to rock units than was measured at surface.

From 270 to 460 meters there are distinct tuffaceous units characterized by medium

grained pale red-pink, magnetic garnet phenocrysts within fine grained black matrix. Contacts of

the garnet tuff unit were 62° TCA on average. From 460 to the end of the hole, the core is dark

pink in colour. This felsic unit looks more similar to the felsic colour banded flows observed in

NA18-01.

All NA18-02 samples within crystal tuffs, ash tuffs and compositionally banded flows

from 29 to 200 meters depth returned Au values below 100 ppb. Sample 522180 returned a

value of 769 ppb Au from 200 to 201 meters within volcaniclastic sediments. The Road Gold

zone occurred within felsic ash and lapilli tuff a few meters after the mafic volcanic contact at

270 meters downhole. Sample 522185 returned a value of 1.5 g/t Au from 278 to 279 meters

depth. The lapilli tuff unit also included quartz vein rich intervals with samples returning 2.4, 1.4,

and 1.7 g/t Au between 280 and 285 meters depth.


NA18-03 was collared approximately 1km north of NA18-01 and NA18-02, at the

western extent of the Spade Lake zone. Drilling began October 23rd and was completed on

October 29th. Preliminary logging was completed between October 24th and Nov 3rd by M Ruhl

and R McEwan of Tri Origin Exploration Ltd. NA18-03 was drilled for 454 meters. Water was

pumped from a north-south running creek that crosses the road.

Target

NA18-03 was drilled to trace the extent and continuity downdip of anomalous gold

assayed in drill core samples from historic Cogema drill holes within the Spade Lake zone. An

IP anomaly was indicated from deep IP survey results, centered at 5483250 meters at surface

on L3600. NA18-03 was collared north of Spade Lake zone to target the downdip extent of the

IP anomaly at approximately 400m downhole, assuming a 70° north dip.

Geology Log Summary

NA18-03 went through 18 meters of overburden, indicating an overburden depth of 16.3

meters, with a drill hole inclination of -65°. From 18 to 209 meters the hole was dominated by a

distinct unit of medium to coarse grained white, subhedral feldspar and grey quartz crystals in a

fine grained dark grey matrix. This unit is classified as feldspar crystal tuff and can be correlated

to previous Tri Origin drill logs, as well as historic logs. This section of core also intersected

amphibole metabasalt and finely laminated volcaniclastic sediments. These units contained nil

to trace sulphides.

15

From 209 to 339 meters, NA18-03 intersected sulphidic ash tuffs with minor intrusions of

the Spade Lake Porphyry. Sericite alteration and blue quartz occurred between 236 and 239

meters depth. A 30 meter continuous section with 3-5% sulphide content occurred from 239 to

269 meters. Sulphide grains were elongated parallel to foliation and in places range up to 10%

of the rock. Foliation was measured between 50 and 60° TCA. From 269 to 284 meters the tuff

contained pale pink, magnetic garnet phenocrysts and nil sulphides. Sulphidic ash tuff continues

after the garnet-rich section, from 284 to 339.3 meters.

The last 115 meters, from 339 to 454 meters, of NA18-03 was dominated by the Spade

Lake Porphyry. The porphyry is characterized by 30-40% medium-coarse grained plagioclase

and quartz phenocrysts in a finer-grained felsic matrix. The unit appeared poorly mineralized

with only occasional weak disseminations of pyrite and minor coarse chalcopyrite clots

associated with the occasional quartz-carbonate veins that cut the unit locally. Towards the end

of the hole the texture of the porphyry transitioned from a quartz-feldspar porphyritic texture to a

red-coloured intrusion with more tightly packed crystals. It is difficult to determine whether the

tightly-packed crystal porphyry intruded adjacent layers of ash tuff as dykes, sills or is crystal

lithic tuff deposited contemporaneously with the tuff layers. There are two intervals less than 10

meters wide with sharp contacts, of ash tuff between 339 meters and the end of the hole which

may represent crystal lithic tuffs.

21 assay samples were taken over the first 239 meters of NA18-03, within white feldspar

crystal tuff units, interbedded amphibole metabasalt and volcaniclastic sediment units, and the

foliated ash tuff unit. All samples within these units contained less than 100 ppb Au. A 53 meter

section from 239 to 292 meters was sampled over 1 meter intervals. The average grade of the

entire ash unit was 147 ppb Au. A comparable average Au content of 120 ppb was returned for

the ash tuff unit from 403.5 to 411 meters within the Spade Lake Porphyry. Quartz veining within

the Spade Lake porphyry from 389.3 to 390 meters returned a single gold assay of 7.8 g/t.

GEOCHEMICAL SUMMARY OVERVIEW

191 samples of drill core were analyzed for gold, and 80 of those were additionally

analyzed for multi-element suite of 49 elements. Of these, 47 samples were analyzed from

NA18-01, 36 from NA18-02, and 108 from NA18-03. Appendix D contains original geochemical

certificates of analysis. Refer to table in Appendix E for a compilation of all gold and multi-

element assay results.

Table 4 lists significant assay results of Au, Ag, Cu, Ni, Cr, As, Zn, Fe, and S. Significant

results were selected based on a preliminary analysis of the spread of data. Additional statistical

analysis is required. Column headings outline the element being analyzed, the unit, and the

detection limit. The table was condensed based on the following criteria, Au ≥ 250 ppb; Ag ≥ 20

ppm; As ≥ 50 ppm; Cu, Ni, Cr, and Zn ≥ 1000 ppm; Fe ≥ 10%; and S ≥ 1%. Upper detection

limits for Zn, Fe, and S are 10 000 ppm, 15%, and 5%, respectively.

NA18-01 returned a maximum assay value of 1450 ppb Au across a 1 metre interval

within a 5.5 metre thick interval of pyritic and sericite-altered rock which averaged 420 ppb Au

starting at 339.5 metres downhole. NA18-02 reported assay values of 1505 ppb Au, 1408 ppb,

16

and 1668 ppb across 1 metre intervals and 2354 ppb from 0.5 wide quartz vein sample within a

7 metre section of core averaging 890 ppb of gold from 278 metres downhole. NA18-03

intersected thick intervals of pyritic and weakly altered rock anomalous in gold abundance. A 53

metre section averaged 150 ppb Au from 239 metres downhole followed by a 16.9 metre

section averaging 120 ppb Au from 318.6 metres downhole. A single high assay of 7833 ppb Au

across 0.7 metres was returned from a quartz vein sample taken at 389.3 metres downhole.

The intervals of sulphidic ash tuff in NA18-03 returned the most notable concentrations

of trace elements. This unit reported values of greater than 900 ppm Cu across 1 metre

intervals from 257 to 259, 275 to 279, and 327to 337 metres downhole. Additionally values of

greater than 500 ppm Zn were reported from approximately 327 to 337 metres downhole, with a

single sample of 1753 ppm Zn from 335 to 335.5 metres. Two samples collected between 246

and 335.5m returned greater than 6 ppm Ag. Sulphur concentrations above the upper detection

limit were also returned from 247 to 331 metres downhole within the sulphidic ash, as well as

values greater than 8% Fe. All drill holes reported negligible values of Ni, Cr, Pb, and As.

17

Table 4. Significant geochemical results, sorted by hole ID then depth.

Hole ID

From m

To m

Length m

Sample No

Au_5_ppm Ag_0.02_ppm Cu_0.5_ppm Ni_0.5_ppm Cr_1_ppm As_1_ppm Zn_1_ppm Fe_0.01_% S_0.01_%

NA18-01 333 334 1 522028 7 0.26 65 65.3 102 1 75 10.3 0.04

NA18-01 339.5 340 0.5 522035 454 1.55 13.8 55.4 64 2 78 4.49 1.67

NA18-01 340 341 1 522036 274 1.36 30.7 79.8 56 1 63 3.65 1.26

NA18-01 343 344 1 522039 1450 6.18 10 162 196 <1 84 4.97 2.02

NA18-01 366 366.8 0.75 522063 83 0.57 1.2 71.6 36 2 25 2.24 1.84

NA18-02 200 201 1 522180 769 - - - - - - - - NA18-02 275 276 1 522182 272 - - - - - - - - NA18-02 278 279 1 522185 1505 1.09 61.1 40.4 43 <1 43 3.96 0.9

NA18-02 280 280.5 0.5 522187 2354 5.46 14.4 44.5 40 1 21 4.78 3.05

NA18-02 282.5 283 0.5 522190 599 1.12 6.6 28 36 <1 25 2.7 1.09

NA18-02 283 284 1 522191 1408 4.11 44.9 29.8 46 <1 29 3.23 1.66

NA18-02 284 285 1 522192 1668 4.91 29.3 49.4 40 <1 71 6.09 3.9

NA18-03 60.6 61 0.4 522150 10 1.05 116 31.1 87 <1 164 7.3 >5

NA18-03 80 81 1 522152 14 3.1 90.5 33.6 97 <1 306 5.04 1.48

NA18-03 82 83 1 522154 6 0.84 43.5 37.7 57 <1 46 4.96 1

NA18-03 109 110.2 1.2 522155 9 0.97 6.2 21.5 32 2 57 2.06 1.15

NA18-03 113 114 1 522159 7 0.18 4.8 19.9 32 1 46 1.97 1.14

NA18-03 114 114.8 0.8 522160 6 0.14 7.7 23.8 40 1 55 2.03 1.2

NA18-03 245 246 1 522083 110 0.79 88.1 21.4 32 3 79 4.46 3.4

NA18-03 246 247 1 522084 135 6.89 562 21.6 27 3 180 6.19 4.23

NA18-03 247 248 1 522085 351 4.33 224 39.2 44 3 77 7.42 5

NA18-03 248 249 1 522086 60 0.77 60.3 18.8 31 3 57 3.63 3.42

NA18-03 253 254 1 522091 208 1.2 327 43.6 58 2 245 7.2 3.96

NA18-03 254 255 1 522092 212 0.88 261 37.1 35 2 139 7.62 >5

NA18-03 255 256 1 522093 119 1.67 393 44.4 49 <1 211 7.39 >5

NA18-03 256 257 1 522094 96 2.35 530 45.1 46 2 392 6.24 4.46

NA18-03 257 258 1 522095 121 1.95 969 46.1 64 1 406 7.6 3.27

NA18-03 258 259 1 522096 124 2.58 919 52.9 79 1 484 8.61 4.28

NA18-03 275 276 1 522113 148 2.74 1975 42.1 91 3 348 3.61 1.01

NA18-03 276 277 1 522114 149 1.7 2375 41.8 101 5 207 4.41 1.19

NA18-03 277 278 1 522115 352 2.61 3512 53.3 80 5 317 5.29 1.55

NA18-03 278 279 1 522116 167 1.9 1594 48.2 96 4 298 4.59 1.18

NA18-03 287 288 1 522125 144 4.17 818 82.3 96 13 787 8.12 >5

NA18-03 288 289 1 522126 134 3.38 967 78.8 116 12 598 7.92 >5

NA18-03 294.8 295.8 1 522196 64 1.35 554 57.6 88 8 380 5.03 2.05

NA18-03 295.8 296.2 0.4 522197 61 1.47 662 55.4 59 7 397 5.34 2.37

NA18-03 327 328 1 522066 123 2.96 979 83.4 70 11 746 12 4.93

NA18-03 328 329 1 522067 128 3.94 905 82 62 9 648 9.67 >5

NA18-03 329 330 1 522072 107 3.89 759 75.8 78 11 574 8.2 4.87

NA18-03 330 331 1 522073 140 2.94 1064 89.5 82 10 494 8.93 >5

NA18-03 331 332 1 522074 102 4.11 901 80.5 76 9 433 7.86 4.82

NA18-03 332 333 1 522075 125 4.08 999 80.7 83 10 491 7.73 4.89

NA18-03 333 334 1 522068 92 2.27 616 87.5 100 13 339 8.48 4.74

NA18-03 334 335 1 522069 70 2.18 821 53.7 84 9 216 5.43 3.23

NA18-03 335 335.5 0.5 522070 99 6.29 2341 28.6 40 5 1753 5.18 4.18

NA18-03 344.8 345.8 1 522195 432 1.47 254 60.1 82 3 129 3.98 1.61

NA18-03 389.3 390 0.7 522194 7833 - - - - - - - -

NA18-03 404 405 1 522142 275 1.92 84.7 35.6 80 2 176 3.46 2.35

NA18-03 405 406 1 522143 125 3.94 122 21.1 72 <1 175 2.3 1.15

NA18-03 407 407.5 0.5 522145 334 - - - - - - - -

18

DRILL SITE COMPLETION

All drill holes were successfully drilled to planned depth, and along planned azimuth and

dip, despite technical difficulties. The Translimit Road was washed out for one week, restricting

all access to and from the drill site. The program encountered multiple equipment failures, at

times with the drill broken down for a few days in a row. Freeze-thaw conditions were harsh on

the condition of the Tomlinson Road and during the program the road was unmaintained by the

forestry company. Ultimately the abnormal wet and cold fall weather ended the drill program

earlier than expected.

All casing was removed from the drill holes upon completion of drilling in a manner such

that overburden material would collapse into the hole. All sites were restored back to clean

condition to minimize any impacts on the surrounding environment.

19

CONCLUSIONS AND RECOMMENDATIONS

Targets were successfully intersected but shallower than the predicted and anticipated

depth. The targeted IP anomalies were confirmed to be the result of auriferous, pyritic rock.

Comparison of historic and current drill results with IP pseudosections indicates that sulphidic

rock extends further down-dip and the stronger parts of IP response are below the depth of

current drilling.

Lithological targets at the Road Gold zone were traced from historic drill holes to NA18-

01. The geologic character of sulphidic, laminated, siliceous ash with minor quartz-sulphide

veins was intersected and confirmed in NA18-01. Au values were lower than expected

compared to historic drill hole intersections located approximately 200m to the east and 150m

up dip. This may limit a westward plunge to the zone.

The expected geological character of the Road Gold zone was not as apparent in NA18-

02. Although significant Au abundance occurred at the same stratigraphic position, alteration in

the form of silica, pyrite, and sericite was less abundant. The other main difference in NA18-02

was the occurrence of an approximately 50m thick sequence of coarse lapilli-bearing fragmental

rock at and immediately south of the expected location of the zone. The effect of this increase in

the thickness of the local stratigraphic sequence on the gold zone is not understood. The mafic

volcanic-felsic volcanic contact which hosts the Road Zone further to the west was intersected

further to the north and further up hole than was expected. Interestingly, the anticipated

eastward projection of the Road Zone was closer to the location of massive sulphide lapilli in

felsic fragmental rock. The gold zone may extend eastward through the felsic fragmental unit

rather than near the mafic-felsic volcanic contact.

From NA18-03, it appears that presence of sulphide within the tuffaceous units at the

Spade Lake zone is laterally continuous; however Au assays returned lower values than

expected based on historic results. An unexpected 70m thick section of weakly pyritic and

weakly altered volcaniclastic rock, averaging over 100 ppb Au was intersected further up hole

than predicted. The expected target was a narrow interval of more pyritic, siliceous, and sericitic

rock. It appears that the gold zone has been diluted and thickened by abundant volcaniclastic

material.

Based on these conclusions the following recommendations are made:

More thorough understanding of structure in the area to better predict lithological

contacts, mineralization signatures, and IP traces at depth

Standardizing historic drill log units with current logs to produce 3D model of all drill

holes

20

REFERENCES

Archer, R.A., 1986, Summary Report of 1986 Winter Field Program, Golden Shield Project –

261, Newmont Exploration of Canada Limited

Harron, G.A., 2005, Qualifying Report on Burntbush Property, Hoblitzell Township, Ontario for

Rockhaven Resources Ltd.

Kendle, F.K., 2012, Report on the 2011 Trenching Program North Abitibi (NA Property), Ministry

of Energy, Northern Development and Mines, Ontario Assessment File Database, file number

20000009080.

Learn, J., 1988a, Final Report 1987 Reverse Circulation Drilling, Burntbush River Project,

Cogema Canada Limited File 87-CDN-47-04.

Learn, J., 1988b, Final Report 1988, Contract Geophysics, Burntbush River Project, Cogema

Canada Limited File 88-CDN-47-02.

Learn, J., 1988c, Final Report 1988 Reverse Circulation Drilling, Burntbush River Project,

Cogema Canada Limited File 88-CDN-47-01.

Learn, J., 1989, Diamond Drill Results 1989 Program, Burntbush River Project, Cogema

Canada Limited, File 89-CDN-47-02.

Learn, J., 1991, Contract Geophysics 1989, 1990, Burntbush River Project, Cogema Canada

Limited File 91-CDN-47-02.

Learn, J., 1992, Final Report 1992 Field Program, Burntbush River Project, Cogema Canada

Limited File # 92-CDN-47-01.

Mandziuk, Z. and Perkins, M., 1997, Report on 1997 Exploration Program Burntbush Project for

Tri Origin Exploration Ltd.

Mandziuk, Z. and Perkins, M., 1998, Report on 1998 Diamond Drill Program, Burntbush Project

for Tri-Origin Exploration Ltd.

Newmont Exploration of Canada Ltd., 1987, Diamond drilling Report # 15, DDHs 261-86-1, 2.

Newmont Exploration of Canada Ltd., 1988, Diamond drilling Report # 18, DDHs 261-87-1 to 8.

Newmont Exploration of Canada Ltd., 1989, Diamond drilling Report # 19, DDHs 261-88-2, 7,

12.

Ruhl, M., McEwan, R., 2019, Report on the 2018 Maping and Sampling Program, North Abitibi

Property, Ministry of Energy, Northern Development and Mines, Ontario Assessment File

Database, report pending approval.

21

PERSONNEL

The following geologists were employed by Tri Origin in the spring and summer of 2018 and

conducted core logging and sampling work on the North Abitibi Property.

Monique Ruhl Contract Geologist Beaverton, Ontario

Rob McEwan Contract Geologist Grand Bend, Ontario

22

STATEMENT OF QUALIFICATIONS

I, Monique Ruhl, of 422 Bay St., Beaverton, ON, do hereby certify that:

1. I am employed as a geologist by Tri Origin Exploration Ltd.

2. I graduated with a bachelor’s degree in earth science (BSc. Geology) from Dalhousie

University in 2016

3. Hold a GIT (Geoscientist-in-Training) membership with the Association of Professional

Geoscientists of Ontario (membership number 10457).

4. I have worked as a geologist for a total of two years.

5. I am responsible for the technical report titled “Report on the Fall 2018 Drill Program

North Abitibi Property”.

6. My knowledge of the property as described herein was obtained by fieldwork and

literature review.

7. I have no direct interest, nor do I expect to receive any interest in the mining claims that

comprise the North Abitibi Property within Hoblitzell Township in the Larder Lake Mining

division.

8. I am not aware of any material fact or material change with respect to the subject matter

of the Technical Report that is not reflected in the Technical Report, the omission to disclose

which makes the Technical Report misleading.

9. I consent to the filing of the Technical Report with any stock exchange and other

regulatory authority and any publication by them for regulatory purposes, including electronic

publication in the public company files on their websites accessible by the public, of the

Technical Report.

Dated this 7th day of March, 2019.

Monique Ruhl

23

I, Robert McEwan, 30 Erin Place, Grand Bend, ON, do hereby certify that:

1. I am employed as a geologist by Tri Origin Exploration Ltd.

2. I graduated with a bachelor’s degree in earth science (BSc. Geology) from Dalhousie

University in 2016

3. I have worked as a geologist for a total of one year.

4. I am responsible for the technical report titled “Report on the Fall 2018 Drill Program

North Abitibi Property”.

5. My knowledge of the property as described herein was obtained by fieldwork and

literature review.

6. I have no direct interest, nor do I expect to receive any interest in the mining claims that

comprise the North Abitibi Property within Hoblitzell Township in the Larder Lake Mining

division.

7. I am not aware of any material fact or material change with respect to the subject matter

of the Technical Report that is not reflected in the Technical Report, the omission to disclose

which makes the Technical Report misleading.

8. I consent to the filing of the Technical Report with any stock exchange and other

regulatory authority and any publication by them for regulatory purposes, including electronic

publication in the public company files on their websites accessible by the public, of the

Technical Report.

Dated this 27th day of November, 2018.

Robert McEwan

APPENDICES

APPENDIX A

LABORATORY PROCEDURES

Minerals Services Revision 0.0

Geochemistry Doc Type Method

Summary

Lakefield Laboratory Method No:

Code GE_FAA313

Service Testing

Minerals Services

Determination Gold by Lead Fusion

Fire Assay and Atomic Absorption

Spectrometry in Exploration samples [30g ; Au; AAS]

Issued Date 02/Sep/2014

Approved by L. Ng

Page 1 of 2 SGS Minerals Services

http://www.geochem.sgs.com/ Member of SGS Group (Société Générale de Surveillance)

1. Parameter(s) measured, unit(s): Gold (Au); in ppb

2. Typical sample size: 30 g

3. Type of sample applicable (media): Crushed and Pulverized rocks

4. Sample preparation technique used: Weighed representative samples are mixed with flux and fused using lead oxide at 1100°C, followed by cupellation of the resulting lead button. The bead is dissolved using HCl and HNO3 and the resulting solution is submitted for analysis

5. Method of analysis used: The digested sample solution is analyzed by Flame Atomic Absorption Spectrometer (AAS).

6. Data reduction by: Computer, on line, data fed to SGS Laboratory Information Management System with secure audit trail.

7. Figures of Merit: This method has been fully validated for the range of samples typically analyzed. Method validation includes the use of reference materials, replicates, duplicates and blanks to calculate accuracy, precision, linearity, range, limit of detection, reporting limit, specificity and measurement uncertainty. The Reporting Limit has been determined according to the following:

Element Reporting Limit (ppb) Upper Limit (ppb)

Au 5.0 10,000

8. Quality control:

Quality control materials include method blanks, duplicates and reference materials and are randomly inserted with the frequency set according to method protocols at ~14%. Quality



control materials will also include BRM (Barren reference materials, or preparations blanks) and replicates if samples have been taken through the sample reduction process. Instrument calibration is performed for each batch or work order and calibration checks are analyzed within each analytical run.

9. Accreditation: The Standards Council of Canada has accredited this test in conformance with the requirements of ISO/IEC 17025. See www.scc.ca for scope of accreditation. Note: Scopes of accreditation are site specific, please check with the local representative.

http://www.scc.ca/



Summary


Code GE_ICM90A

Service Testing

Minerals Services

Determination of Fifty-five (55) Elements in

Exploration Samples using Sodium Peroxide

Fusion and a Combination of Inductively

Coupled Plasma Optical Emission

Spectrometry (ICP-OES) and Inductively

Coupled Plasma Mass Spectrometry (ICP-

MS) [Na2O2; HN03; C4H6O3; Ag, Al; As; Ba; Be; Bi;

Ca; Cd; Ce; Co; Cr; Cs; Cu; Dy; Er; Eu; Fe; Ga; Gd; Ge; Hf; Ho; In; K; La; Li; Lu; Mg; Mn; Mo; Nb; Nd; Ni; P; Pb; Pr; Rb; Sb; Sc; Sm; Sn; Sr; Ta; Tb; Th; Tl; Ti; Tm; U; V; W; Y; Yb, Zn; Zr]

Issued Date 13/Jul/2015

Approved by S. Meyers



1. Parameter(s) measured, unit(s): Silver (Ag); Arsenic (As); Barium (Ba); Beryllium (Be); Bismuth (Bi); Cadmium (Cd); Cerium (Ce); Cobalt (Co); Chromium (Cr); Cesium (Cs); Copper (Cu); Dysprosium (Dy); Erbium (Er); Europium (Eu); Gallium (Ga); Gadolinium (Gd); Germanium (Ge); Hafnium (Hf); Holmium (Ho); Indium (In); Lanthanum (La); Lithium (Li); Lutetium (Lu); Manganese (Mn); Molybdenum (Mo); Niobium (Nb); Neodymium (Nd); Nickel (Ni); Lead (Pb); Praseodymium (Pr); Rubidium (Rb); Antimony (Sb); Scandium (Sc); Samarium (Sm); Tin (Sn); Strontium (Sr); Tantalum (Ta); Terbium (Tb); Thorium (Th); Thallium (Tl); Thulium (Tm); Uranium (U); Vanadium (V); Tungsten (W); Yttrium (Y); Ytterbium (Yb); Zinc (Zn); Zirconium (Zr), in ppm Aluminum (Al); Calcium (Ca); Iron (Fe); Potassium (K); Magnesium (Mg); Phosphorus (P); Titanium (Ti) in % Boron (B), Selenium (Se), Tellurium (Te) in ppm and Sulfur (S) and Silica (Si) in % can be added as additional

2. Typical sample size: 0.1 g

3. Type of sample applicable (media): Crushed and Pulverized rocks, soils and sediments

4. Sample preparation technique used: Weighed representative samples are digested fused in glassy carbon crucibles using sodium peroxide (Na2O2). The resultant cake is dissolved in HNO3.

5. Method of analysis used: The digested sample solution is analyzed by inductively coupled plasma Mass Spectrometer (ICP-MS) and inductively coupled plasma Optical Emission Spectrometer (ICP-OES).

6. Data reduction by: Computer, on line, data fed to SGS Laboratory Information Management System with secure audit trail.



7. Figures of Merit: This method has been fully validated for the range of samples typically analyzed. Method validation includes the use of reference materials, replicates, duplicates and blanks to calculate accuracy, precision, linearity, range, limit of detection, reporting limit, specificity and measurement uncertainty. The Reporting Limit has been determined according to the following:

Element

Reporting

Limit

(ppm)

Upper

Limit Element

Reporting

Limit

(ppm)

Upper

Limit Element

Reporting

Limit

(ppm)

Upper

Limit Element

Reporting

Limit

(ppm)

Upper

Limit

Ag 1.00 0.1% Er 0.05 0.10% Mn 10 10% Ta 0.5 1.0%

Al 0.01(%) 25% Eu 0.05 0.10% Mo 2.00 1.0% Tb 0.05 0.10%

As 5.00 10% Fe 0.01(%) 25% Nb 1.00 1.0% Th 0.10 0.10%

Ba 10 1.0% Ga 1.00 0.10% Nd 0.10 1.0% Ti 0.01(%) 25%

Be 5.00 0.25% Gd 0.05 0.10% Ni 5.00 1.0% Tl 0.50 0.10%

Bi 0.10 0.10% Ge 1.00 0.10% P 0.01(%) 25% Tm 0.05 0.10%

Ca 0.1(%) 25% Hf 1.00 1.0% Pb 5.00 1.0% U 0.05 0.1%

Cd 0.20 1.0% Ho 0.05 0.10% Pr 0.05 0.1% V 5.00 1.0%

Ce 0.10 1.0% In 0.20 0.10% Rb 0.20 1.0% W 1.00 1.0%

Co 0.50 1.0% K 0.1(%) 25% Sb 0.10 1.0% Y 0.50 0.1%

Cr 10 5% La 0.10 1.0% Sc 5.00 5.0% Yb 0.10 0.1%

Cs 0.10 1.0% Li 10 5.0% Sm 0.10 0.1% Zn 5.00 1.0%

Cu 10 1.0% Lu 0.05 0.10% Sn 1.00 1.0% Zr 0.50 1.0%

Dy 0.05 0.1% Mg 0.01(%) 25% Sr 10 0.5%

B 10 10% S 0.01 35% Se 0.2 0.1% Si 0.1(%) 35%

Te 0.1 0.1%

8. Quality control:

Quality control materials include method blanks, duplicates and reference materials and are randomly inserted with the frequency set according to method protocols at ~14%. Quality control materials will also include BRM (Barren reference materials, or preparations blanks) and replicates if samples have been taken through the sample reduction process. Instrument calibration is performed for each batch or work order and calibration checks are analyzed within each analytical run.

9. Accreditation: The Standards Council of Canada has accredited this test in conformance with the requirements of ISO/IEC 17025. See www.scc.ca for scope of accreditation. Note: Scopes of accreditation are site specific, please check with the local representative.

http://www.scc.ca/



Summary


Code GO/GC/GT_XR

F76V

Service Testing

Minerals Services

Preparation and Determination of

Major Element Oxides, LOI and Rare

Earth Oxides by Borate Fusion and

Xray Fluorescence Spectrometry [SiO2, Al2O3, Fe2O3, MgO, CaO, Na2O,

K2O, P2O5, MnO, TiO2, Cr2O3; V2O5; LOI; additions BaO; Ce2O3; Nd2O3, La2O3; Pr2O3,

Sm2O3; Nb2O5,ThO2, Ta2O5; SnO2; SrO; ZrO2; HfO2; Y2O3; WO3; U3O8; Co; Ni ; XRF]

Issued Date 23/Sep/2014

Approved by K. Patel



1. Parameter(s) measured, unit(s):

Silicon Dioxide (SiO2), Aluminum Oxide (Al2O3), Iron(III) Oxide (Fe2O3), Magnesium Oxide (MgO), Calcium Oxide (CaO), Sodium Oxide (Na2O), Potassium Oxide (K2O), Phosphorus Pentoxide (P2O5), Manganese Oxide (MnO), Titanium Dioxide (TiO2), Chromium (III) Oxide (Cr2O3), Vanadium Oxide (V2O5), LOI, in % Barium Oxide (BaO), Cerium (III) Oxide(Ce2O3), Neodymium Oxide (Nd2O3), Lanthanum Oxide (La2O3), Praseodymium Oxide (Pr2O3), Samarium Oxide (Sm2O3), Niobium Pentoxide (Nb2O5), Thorium Dioxide (ThO2), Tantalum Pentoxide (Ta2O5), Tin Dioxide (SnO2) Uranium Oxide (U3O8), Cobalt (Co), Nickel (Ni), Strontium Oxide (SrO), Zirconium Dioxide (ZrO2), Hafnium Oxide (HfO2), Yttrium Oxide (Y2O3), Tungsten Trioxide (WO3) in % can be added as additions

2. Typical sample size: 0.2 to 0.5g

3. Type of sample applicable (media): Rocks, oxide ores, concentrates and catalysts

4. Sample preparation technique used: Samples are crushed and pulverized according to client specified instructions or default preparation procedures. This method is used to report, in percentage, the whole rock suite (SiO2, Al2O3, Fe2O3, MgO, CaO, Na2O, K2O, P2O5, MnO, TiO2, Cr2O3 ,V2O5 ). Sample preparation entails the formation of a homogenous glass disk by the fusion of the sample and a lithium tetraborate/lithium metaborate mixture. The LOI is determined separately and gravimetrically at 1000°C.

5. Method of analysis used: The prepared disks are analyzed by wavelength dispersion X-ray fluorescence (WD-XRF). The LOI is included in the matrix correction calculations, which are performed by the XRF software.



6. Data reduction by: Computer, on line, data fed to Laboratory Information Management System with secure audit trail. .

7. Figures of Merit: This method has been fully validated for the range of samples typically analyzed. Method validation includes the use of reference materials, replicates, duplicates and blanks to calculate accuracy, precision, linearity, range, limit of detection, reporting limit, specificity and measurement uncertainty.

Element

Report Limit

%

SiO2 0.01 Al2O3 0.01 MgO 0.01 Na2O 0.01 K2O 0.01 CaO 0.01 P2O5 0.01 TiO2 0.01 Cr2O3 0.01 V2O5 0.01 Fe2O3 0.01 MnO 0.01 LOI -10

*upper limit for all elements is 100%. A negative LOI indicates a gain on ignition

8. Quality control: Quality control materials include method blanks, duplicates and reference materials and are randomly inserted with the frequency set according to method protocols at ~14% for exploration and ore grade analysis and 20% for process control analysis. Quality control materials will also include BRM (Barren reference materials, or preparations blanks) and replicates if samples have been taken through the sample reduction process. Party quality samples are assayed in duplicate, umpire quality samples are in triplicate. Calibration materials that cover the range upon method set-up; calibration check performed daily.

9. Accreditation: The Standards Council of Canada has accredited this test in conformance with the requirements of ISO/IEC 17025. See www.palcan.scc.ca for scope of accreditation. Note: Scopes of accreditation are site specific, please check with the local representative.

http://www.palcan.scc.ca/

APPENDIX B

DRILL LOGS

NA18-01

LoggingPROJECT: North Abitibi 2018 PROJECTION: UTM NAD 83 Zone 17 DIP: -72 DATE BEGAN: 27-Sep-18HOLE NO.: NA18-01 NORTHING: 5482351 AZIMUTH: 170 DATE COMPLETED: 10-Oct-18

TARGET: Extending historic gold zone EASTING: 576301 TOTAL DEPTH: 464m LOGGED BY: along strike at depth ELEVATION: 300m CORE SIZE: NQ DRILLED BY:

mFrom mTo DESCRIPTION mFrom mTo LITHOLOGY MINERALIZATION ALTERATION TYPE TCA SAMPLE # mFrom mTo mLength Description0 5 Overburden5 331 Mafic Metavolcanics Interbedded amphibole metabasalt and tuffs

Grey, chlorite-rich, well foliated interbedded mafic tuffs with medium to coarse grained flows. Cross-cutting and bedding parallel quartz veins throughout. Most sulphide bearing veins are quartz-carbonate. Three main textures that are interbedded on a scale of less than 5m. 1) Fine grained cystal tuff with thin (<0.5mm) chlorite-rich beds, 2) porphyritic medium grained flow with green-grey amphibole crystals in a finer grained light grey matrix 3) quartz veinlet rich tuffaceous sections, running parallel to foliation, rock is light coloured.

Nil to trace sulphides overall, some sections (<2m) with trace disseminated sulphides parallel to foliation. Trace to 3% sulphides in quartz veins. Sulphide content increaseses with depth.

Greeny white micaceous mineral along quartz veins and fractures at ~70m and 124m depth.

132 143 Interbedded amphibole metabasalt and tuffs 1% disseminated sulphides parallel to foliation and 1-3% within quartz veins in porphyritic crystal tuff.

foliation (143m) 54 522044 137 137.3 0.3 QV with sulphides

143 151 Interbedded amphibole metabasalt and tuffs

151 157 Ash tuff- Fine grained well foliated light grey material 522045 157.1 157.3 0.2 QV with sulphides

157 174 Interbedded amphibole metabasalt and tuffs Very strongly magnetic thin beds of very fine grained black mineral (magnetite).

foliation (165m) 55

174 185 Porphyritic and well-foliated. Phenocrysts of needle-like biotite in chlorite-rich matrix.

185 218 Interbedded amphibole metabasalt and tuffs 1-3% disseminated, lamiated py/po from 212 to 218m.

foliation(194m) 64 522046522047522048522049522050

212213214215216

213214215216217

1 V FG diss, foliated sulphides and thin, <2cm, QVs with sulphides''''''''

218 222 Lapilli tuff- 1-4cm elongated lapilli fragments and 25mm circular phenocrysts in fine grained light grey matrix. foliation (221m) 58

222 235 Amphibole Metabasalt- Medium grained porphyritic flow. Black prismatic amphibole crystals in medium grained matrix. Flow banded sections (light and dark grey), Minor qtz veinlets, variably interbedded with thinly laminated volcaniclastics sediments.

522210522211

222223

223224

1 Trace sulphides with quartz veinlets + chlorite''

235.3 237.5 Garnet Tuff- <0.5mm subhedral garnet crystals in fine grained grey matrix. Garnet crystals

237.5 243 Amphibole Metabasalt- Medium grained porphyritic flow. Black prismatic amphibole crystals in medium grained matrix. Flow banded sections (light and dark grey). Less chloritic than previous mafic volcanic units. Minor quartz (less carbonate) veins and veinlets. Gradual bottom contact to more silicious volcanics with quartz veins.

Narrow intervals of laminated qtz-carbonate veining with tourmaline and pyrite.

foliation (241m) 68

243 245 Crystal tuff- Medium grained, foliated, elongated crystals in a fine dark grey matrix 522051 244 245 1 QV with sulphides

245 250 Amphibole Metabasalt- Medium grained porphyritic flow. Black prismatic amphibole crystals in medium grained matrix. Light and dark grey flow banded sections. Minor qtz veinlets, variably interbedded with thinly laminated volcaniclastics sediments.

250 253 Fault- orientation unknown 522052 251 253 2 QVs with sulphides and red/lime green alteration/mineralization throughout section

253 284 Interbedded amphibole metabasalt and tuffs foliation (272m) 61 522053 278.5 279 0.5 QV with sulphides

284 297 Volcaniclastic sediments- Fine grained, thinly banded volcanics. Dark grey and purply-brown alternating bands (biotite-rich?). Trace magnetic sulphides.

foliation (296m) 69

297 323 Interbedded amphibole metabasalt and tuffs

323 331 Fe-carbonate unit (?)- Fine to medium grained mafic volcanic with transitional bottom contact with felsic volcanics.

Fe-carbonate minerals foliation (329m) 62 522025 330 331 1 Area above sulphide zone

331 411.6 Felsic Metavolcanics Interbedded felsic banded tuffs and porphyritic crystal tuffsInterbedded siliceous tuffs and porphyritic crystal tuffs with gradual contacts. Potassium feldspar-rich sections- large felsic blocks/bombs that have been flattened and extend across the whole core. Quartz veins throughout, max width of 50cm.

1-3% disseminated sulphides and sulphides in quartz veins throughout.

331 339.5 Ash Tuff- Felsic ash with minor blue quartz eyes. 522026522027522028522029522030522031522032522033522034

331332333334335336337338339

332333334335336337338339339.5

111111110.5

Area above sulphide zoneArea above sulphide zone with ~3cm qtz veinArea above sulphide zone with 2 ~1cm qtz veinsArea above sulphide zone with thin scattered veiningArea above sulphide zoneArea above sulphide zone with trace garnet or sphaleriteArea above sulphide zone with trace garnet or sphaleriteArea above sulphide zone with trace sulphidesTrace sulphides

PRIMARY ROCK TYPE STRUCTUREPRIMARY ROCK UNIT

Tri Origin Exploration LtdDiamond Drill Log

SAMPLE INTERVAL

Drilling26-Sep-1804-Oct-18M. Ruhl and R. McEwanVital Driling

Page 1 of 2

NA18-01

mFrom mTo DESCRIPTION mFrom mTo LITHOLOGY MINERALIZATION ALTERATION TYPE TCA SAMPLE # mFrom mTo mLength Description

PRIMARY ROCK TYPE STRUCTUREPRIMARY ROCK UNIT SAMPLE INTERVAL

339.5 367 Colour banded tuff- Finely laminated grey and greeny-red bands. Sericite alteration and salmon-pink mineral alteration minor blue quartz eyes. Brecciated from 345.3 to 345.5m depth. Red angular clasts in fine grained green-black matrix. Thin beds, <20cm, of porphyritic unit with pink phenocrysts.

3-5% disseminated, euhedral pyrite from 339.5 to 347m.

Sericite alteration compositional banding (353m)

55 522035522036522037522038522039522040522041522042522043522054522055522056522057522058522059522060522061522062522063522064

339.5340341342343344345346346.5347348349350351352353354365366366.75

340341342343344345346346.5347348349350351352353354355366366.75367.75

0.51111110.50.51111111110.751

3-5% disseminated sulfides in qtz vein3-5% disseminated sulfides in qtz vein1-3% disseminated sulfides in qtz veinTrace sulphides5-10% cubic pyrite, salmon colour groundmass, nil qtz vein3-5% cubic pyrite, salmon groundmass, few qtz veinstrace cubic pyrite, pink groundmass, no qtz veins1-3% suflides, pink groundmassTrace sulphides, no pinkTrace sulphides in porph FV, blue quartz eyesTrace sulphides in porph FVTrace sulphides in porph FV, some quartz veinlets with sulphidesTrace sulphides in porph FVNil to trace sulphidesTrace sulpides in pink and grey banded FVTrace sulpides in pink and grey banded FVTrace sulpides in pink and grey banded FV3-5% diss sulphidesQtz vein with sulphides, green alterationIntermediate groundmass with felsic porphy- in contact with QV with sulphides

367 385.5 Porphyritic crystal tuff- Light grey subhedral phenocrysts, ~2mm, in a fine grained darker grey matrix.

385.5 409.5 Colour banded tuff- Back to finely laminated grey and greeny-red bands but without sercite alteration or as many sulphides. Red in colour, not salmon.

compositional banding (399m)

58 522212522213522214522215

390403404405

391404405406

1 Trace sulphides- py veiningRed alterationRed alterationRed alteration

409.5 411.6 Porphyritic crystal tuff- Back to grey porphyritic flow unit.

411.6 464 Intermediate Metavolcanics

Compositionally banded flowsSharp upper contact. Alternating beds of light and dark grey fine grained material- light grey overall. Well foliated. Possible black lapilli fragments in upper 2m. Elongated fragments, max 3cm long.

foliation (413m)foliation (425m)

6047

522065 416 417.4 1.4 Fine grained disseminated py/po and QVs

429 432 Compositionally banded flows 1-3% disseminated py/po in QVs Quartz veins, max 10cm wide

432 443 Compositionally banded flows foliation (438m) 47

443 449 Compositionally banded flows 3-5% disseminated py/po in QVs Quartz veins, max 35cm wide

449 452 Compositionally banded flows452 454 Compositionally banded flows Brick red mineral staining along fractures

454 459 Compositionally banded flows foliation(459m) 44

464 EOH

Page 2 of 2

NA18-02

LoggingPROJECT: North Abitibi 2018 PROJECTION: UTM NAD 83 Zone 17 DIP: -64 DATE BEGAN: 10-Oct-18HOLE NO.: NA18-02 NORTHING: 5482436 AZIMUTH: 170 DATE COMPLETED.: 21-Oct-18

TARGET: Base of road gold zone and EASTING: 576705 TOTAL DEPTH: 470 LOGGED BY: IP anomaly at ~300m ELEVATION: 297m CORE SIZE: NQ DRILLED BY: downhole

mFrom mTo DESCRIPTION mFrom mTo LITHOLOGY MINERALIZATION ALTERATION TYPE TCA SAMPLE # mFrom mTo mLength Description0 19 Overburden

19 39 Mafic Metavolcanics 19 23 Crystal TuffMassive, tightly packed medium to coarse grained quartz and pale pink feldspar phenocrysts in finer grained black matrix. Very sharp bottom contact. Nil sulphides overall, except at 19.5m there are two 'clasts' with 1-3% py/po. Clasts are ~5cm x 3cm and look like cluster of the same pink feldspar mineral. No distinguisable crystal habit. Sharp bottom contact.

23 39 Ash TuffFine grained, dark grey, well-foliated tuffs. Quartz veinlets running parallel to foliation throughout.

foliation (33m)foliation (37m)

5645

23.5 26.5 Fault- Orientation unknown. Broken and missing core.

39 94 Intermediate Metavolcanics

39 94 Banded flowsVery fine grained, pale grey, compositional banded intermediate volcanic flows. Nil sulphides overall.

compositional banding (61m)compositional banding (85m)

3736

522165522166522167522168522169522170522171522172522173522174522175

3939.540.541.542.5438586878889

39.540.541.542.543448687888990

0.51110.5111111

QV with sulphide, gnts, and green mineralTrace sulphides and gntTrace sulphides and gntTrace FG sulphidesQV with sulphides and green mineralTrace sulphidesQV w/ sulphides and iron oxide stainingTrace sulphides, qv's, iron oxide stainingTrace sulphides, qv's, iron oxide stainingTrace sulphides, qv's, iron oxide stainingTrace sulphides, qv's, iron oxide staining

39 44 Banded flows Trace sulphides in quartz veins. Euhedral, pale pink garnet cyrstals. Dark red mineral clusters, 1x1cm, at 44m depth (sphalerite?).

49.8 94 Banded flows- Buff green grey and pale red bands, <10cm wide, within grey beds. More felsic in composition. Trace sulphides near and within QV.

94 270 Mafic Metavolcanics and volcaniclastic

sediments

94 108.6 Crystal TuffFine grained, laminated white and dark grey <5mm wide beds with elongated chlorite crystals parallel to foliation. Beds deformed around quartz veins.

108.6 137.3 Amphibole MetabasaltMedium to coarse grained, dark green amphibole phenocrysts in fine grained grey matrix. Foliated. Nil sulphides.

foliation (124m) 48

137.3 206 Volcaniclastic sediments and mafic tuffs Mainly very fine grained, chlorite-rich volcaniclastic sediments interbedded with tuffs and minor flows. Gradual contacts and frequently alternating textures. 1) Purply-brown beds and chlorite-rich alternating beds. 2) Finely laminated, deformed tuffaceous ash beds. 3) Fine grained bedded sections with angular clasts, clasts are <5mm long. 4) Minor needle-like black amphibole phenocyrstic flows. Nil to trace sulphides overall.

sharp contact (137.3m) 48 522176522177522178522179522180

164195.7198199200

165196.2199200201

10.5111

QV w/ sulphides and black mineralsQV w/sulphides and chloriteTrace fine grained disseminated sulphides with chloriteTrace fine grained disseminated sulphides with chloriteTrace fine grained disseminated sulphides with chlorite

154 164 Volcaniclastic sediments and mafic tuffs Trace, non-continuous very fine grained foliated disseminated sulphides.

203 205 Garnet Tuff Subhedral, 3mm garnet phenocrysts.205 257 Amphibole Metabasalt

Fine grained chloritie-rich matrix with medium grained black needle-like, randonly oriented amphibole phenocrysts. Minor thin, fine grained interflow sediments. Nil to trace sulphides. Gradual bottom contact, interbedded until ~275m with unit below. Beds of flow are <0.5m.

257 270 Volcaniclastic sediments and mafic tuffsInterbedded fine grained purply-brown alternating with chlrorite-rich beds with minor laminated garnet tuffs.

264 264.5 Garnet tuff Subhedral, 3mm garnet phenocrysts.

PRIMARY ROCK UNIT


SAMPLE INTERVAL

Drilling08-Oct-1819-Oct-18M. Ruhl and R. McEwanVital Driling

PRIMARY ROCK TYPE STRUCTURE

Page 1 of 2

NA18-02


PRIMARY ROCK UNIT SAMPLE INTERVALPRIMARY ROCK TYPE STRUCTURE

270 470 Felsic Metavolcanics 270 292.9 Lapilli tuffFine grained alternating light grey/blue and pale green bands with subangular, elongated clasts throughout. Clasts range from <5mm to 70mm long. Larger heterolithic clasts, as well as smaller cherty-looking fragments. Clasts of massive sulphides from 313.8-323m depth. Thin beds, <2cm, of buff coloured crystal ash tuffs. Black needle-like minerals within fine grained buff matrix.

522181522182522183522184522185522186522187522188522189522190522191522192522193

274275276277278279280280.5281.5282.5283284285

275276277278279280280.5281.5282.5283284285286

1111110.5110.5111

Trace sulphides above pyritic zoneTrace sulphides above pyritic zoneTrace sulphides above pyritic zoneTrace sulphides above pyritic zone; possible fault3% py/po3% py/poQV w/ sulphidesTrace fine grained disseminated sulphides Trace fine grained disseminated sulphides Trace sulphides w/ QV1-3% sulphides w/QV1-3% sulphides w/QVTrace sulphides; fragmental felsic volcanic

270 279.5 Section of massive to finely laminated ash tuff with quartzo-feldspathic veining with sulphides throughout. <0.5m sections of subhedral pale pink, garnet phenocrysyts, ~5mm in diameter.

1-3% fine grained disseminated py/po and along quartz veinlets running parrallel to foliation.

279.5 285.5 Lapilli Tuff 3-5% disseminated py/po and 5% along quartzofeldspathic veins. At 284m, clasts 5x7cm of py within quartzo-feldspathic veins. Section looks similar to high Au zone in NA07-02.

292.9 313.8 Garnet Tuff- Fine grained banded mauve/green volcaniclastic sediments with garnet phenocrysts. compositional banding (299m) 44

313.8 323 Lapilli Tuff Massive sulphide clasts. Max 10cm wide at 323m depth.

522204522205522203

316317322.5

317318323.5

111

QVs with green mineral and clasts of MSClasts of MSQVs with green mineral and clasts of MS

323 418 Lapilli Tuff foliation (347m) 43 522206522207522208522209

334.5335.5336.5337.5

335.5336.5337.5339

1111.5

Trace sulphides with minor QVsTrace sulphides with minor QVsTrace sulphides with QVsTrace sulphides with QVs

418 460.5 Interbedded banded flows and garnet tuffsTop contact marked by 30cm buff brown crystal tuff with angular fragments. Unit consists of repeating, parallel thin beds, <5cm, alterating between fine grained steel-blue beds and black to dark grey beds. Distinct tuffaceous unit with medium grained pale redy-pink garnet phenocrysts within fine grained black matrix. Minor black lapilli fragments at bottom. Gradual bottom contact. Nil sulphides overall, trace in some quartz veins.

Beds of subhedral, 3mm garnet phenocrysts.

bedding (430m) 62

460.5 470 Pink Lapilli TuffDark pink, fine grained angular fragments within fine grained black matrix. Core looks banded- fragments flattened/large enough to go through the whole core. Looks like felsic unit in NA18-01 @ 339.5m but without sulphides.

466.5 470 Blue quartz eyes, 1-3mm in diameter.

470 EOH

Page 2 of 2

NA18-03

LoggingPROJECT: North Abitibi 2018 PROJECTION: UTM NAD 83 Zone 17 DIP: -65 DATE BEGAN: 24-Oct-18HOLE NO.: NA18-03 NORTHING: 5483476 AZIMUTH: 170 DATE COMPLETED.: 03-Nov-18

TARGET: Extension of Spade Lake Au EASTING: 576302 TOTAL DEPTH: 454m LOGGED BY: Zone along strike at depth. ELEVATION: 292 CORE SIZE: NQ DRILLED BY: IP anomaly at ~400m depth.

mFrom mTo DESCRIPTION mFrom mTo LITHOLOGY MINERALIZATION ALTERATION TYPE TCA SAMPLE # mFrom mTo mLength Description0 18 Overburden

18 209 Mafic Metavolcanics and volcaniclastic

sediments

18 59.5 White Feldspar Crystal TuffMedium to coarse grained white, subhedral feldspar and grey quartz crystals in a fine grained dark grey matrix. Minor blue quartz crystals. Phenocrysts are randomly oriented, massive texture. Black, angular fragments, 5-7cm long, at 32 and 59m depth. Nil sulphides. Sharp bottom contact.

59.5 119.5 Amphibole metabasalt and minor volcaniclastic sedimentsMostly gradual contacts, except for sharp contacts at 68, 70.4, and 88m. Units alternate on a scale of <10cm up to 1.5m. Flows have medium-grained, greeny-black, needle-like amphiboles in fine grained chlorite-rich matrix. Sediments are finely banded, fine-grained, purply-brown and grey beds. With nil to trace sulphides in beds. 1-3% py/po in some quartz veins. Gradual bottom contact.

sharp contact (59.5m)sharp contact (67.8m)compositional banding & mineral elongation (70.5m)compositional banding (87.3m)Sharp contact (88m)

4858

505660

522150522151522152522153522154522155522156522157522158522159522160522161522162522163522164

60.679808182109110.2111112113114114.8116117118

6180818283110.2111112113114114.8116117118119

0.411111.20.81110.81.2111

QV with sulphidesTrace FG disseminated sulphides in brown and purple seds''''''Trace FG disseminated sulphides in white feldspar xl tuffTrace FG disseminated sulphides in green amph metabasalt''''Trace FG disseminated sulphides in white feldspar xl tuff1-3% sulphides in white feldspar xl tuffTrace sulphides and red mineral along veins green amph metabasalt''''1-3% sulphides and red mineral in green amph metabasalt

78.5 84.5 Volcaniclastic sediments- Very fine grained, finely laminated, purply-brown sediments. Sharp top and bottom contacts.

compositional banding (83m) 53

91.6 94 Volcaniclastic sediments- Very fine grained, finely laminated, grey-brown to blue sediments. Interbedded with <2cm thick green amphibole-rich beds. Beds appear to be folded and deformed. Potential cross-bedding, indicating way-up is up the hole.

109 119.5 Amphibole metabasalt and minor volcaniclastic sediments 1-3% fine-grained, laminated py/po and medium grained py/po along quartz veins.

compositional banding & elongated sulphides (115m) 70

119.5 154.5 White Feldspar Crystal TuffSame unit as top of hole. Medium to coarse grained white, euhedral phenocrysts in a fine grained dark grey matrix. Nil sulphides overall, trace at top contact.

126 134 Fault zone, broken core. Orientation unknown. 154.5 209 Interbedded white felspar crystal tuff and ash tuff

Interbedded 50/50 of white and pink feldspar crystal tuff and very fine grained ash tuff. Alternating on scale of <025cm. Ash tuff is finely banded and contains medium grained blue quartz-eyes throughout. Trace sulphides throughout. 1m gradual transition at ~210m to pink crystalline section at end of unit.

209 339.3 Mafic sulphidic tuffs intruded by porphry

209 236 Sheared Ash TuffsFine grained, dark grey to black tuffaceous material (ash and crystal tuffs). Indications of shear texture from elongated lithic fragments, sigma structures, and strain shadows. Black, angular, 3cm long fragment at 231.5m depth. Elongated parallel to foliation

522198522199522200522201522202522076

225226227228229232.5

226227228229230233.5

1 Ash tuff- 1-3% elongated sulphides''''''''''

210 215 Spade Lake PorphryPotasium feldspar-rich sill. Medium to coarse grained, pink feldspar and quartz-rich. Sharp contacts.

236 239 Pink Crystal TuffFine grained, siliceous, pale pink and buff bands with medium grained blue quartz-eyes. Serecitic alteration.

Sericite alteration

239 296 Interbedded ash and garnet tuffsFine grained, well-foliated, dark grey tuffaceous. Blue quartz-rich from 239 to 245m depth. Medium grained pale pink, strongly magenetic garnet crystals in continuous segments starting at ~269m depth.

foliation & elongated sulphides (246m)foliation & elongated sulphides (267m)

60

50

PRIMARY ROCK UNIT


SAMPLE INTERVAL

Drilling23-Oct-1829-Oct-18M. Ruhl and R. McEwanVital Driling

PRIMARY ROCK TYPE STRUCTURE

Page 1 of 3

NA18-03



239 269 Ash tuff 3-5% disseminated, medium grained yellow sulphides.

522077522078522079522080522081522082522083522084522085522086522087522088522089522090522091522092522093522094522095522096522097522098522099522100522101522102522103522104522105522106

239240241242243244245246247248249250251252253254255256257258259260261262263264265266267268

240241242243244245246247248249250251252253254255256257258259260261262263264265266267268269

111111111111111111111111111111

Ash tuff - 1-3% sulphidesAsh tuff - 1-3% sulphidesAsh tuff - 3-5% sulphidesAsh tuff - 3-5% sulphidesAsh tuff - 5-10% sulphides w/qtz veinletsAsh tuff - 5-10% sulphides w/qtz veinletsAsh tuff - 1-3% disseminated sulphides w/heavy serecite alterationAsh tuff - 5-10% sulphides w/qtz veinletsAsh tuff - 5-10% sulphidess w/qtz/kfeld veinletsAsh tuff - 3-5% disseminated sulphides w/heavy serecite alterationAsh tuff - 5-10% sulphidessAsh tuff - 3-5% disseminated sulphides w/ 5cm qtz veinAsh tuff - 3-5% sulphidesAsh tuff - 3-5% sulphidesAsh tuff - 5-10% sulphides in deformed bedsAsh tuff - 5-10% sulphides in deformed bedsAsh tuff - 3-5% sulphidesAsh tuff - 3-5% sulphidessAsh tuff - 5-10% sulphides in deformed bedsAsh tuff - 5-10% sulphidesAsh tuff - 3-5% sulphidesAsh tuff - 3-5% sulphides +gntAsh tuff - 3-5% sulphidesAsh tuff - 1-3% sulphidesAsh tuff - 1-3% sulphidesAsh tuff - 1-3% sulphidesAsh tuff - 1-3% sulphidesAsh tuff - 1-3% sulphidesAsh tuff - 1-3% sulphides + gntAsh tuff - 1-3% sulphides

245 245.6 Ash tuff Strong sericite alteration. Rock is pale greeny-white, well-foliated.

248 249 Ash tuff Strong sericite alteration. Rock is pale greeny-white, well-foliated.

269 284 Garnet tuff- Repearting garnet-rich beds. Subhedral, 3mm garnet phenocrysts. folation & elongated sulphides (272m)folation & elongated sulphides (278m)

5652

522107522108522109522110522111522112522113522114522115522116522117522118522119522120522121

269270271272273274275276277278279280281282283

270271272273274275276277278279280281282283284

111111111111111

Ash tuff - 3-5% sulphides +gntAsh tuff - 1-3% sulphides''''''''Ash tuff - 1-3% sulphides +gnt''''''''''''''''

284 292.8 Ash tuff 3-5% disseminated, medium grained yellow sulphides.

522122522123522124522125522126522127522128522129522130

284285286287288289290291292

285286287288289290291292292.5

111111110.5

Ash tuff - 1% sulphides +gntAsh tuff- 3-5% sulphides''''''''''''''

292.8 294.5 Spade Lake PorphryPotasium feldspar-rich phenocrysts in black matrix.

294.5 296 Ash tuff 3-5% disseminated, medium grained yellow sulphides.

Bedding (295m) 57 522196522197

294.8295.8

295.8296.2

10.4

Ash tuff with blue quartz eyes- 1-3% sulphides''

296 315.2 Spade Lake PorphryMassive, medium to coarse grained, rounded pink feldspar and quartz phenocrysts in fine grained black matrix. Blue quartz-eyes rich. Top meter looks like mixture of sulphide-rich unit and porphyry.

Contact (296m) 54

315.2 335.8 Interbedded ash and garnet tuffsSame as previous unit. Foliated ash tuff. Minor lapilli fragments. Beds of pale pink, magnetic garnet crystals. Disseminated sulphides throughout. Micro faults throughout. Broken bottom contact (fault?).

Beds of garnet 522131522132522133522134522135522136522137522138522139522140522066522067522072522073522074522075522068522069522070

315.2316.2318.6319.6321322323324325326327328329330331332333334335

316.2317.2319.6321322323324325326327328329330331332333334335335.5

1111.4111111111111110.5

Ash tuff- 3-5% sulphides and QV with sulphides''Ash tuff- 1-3% sulphidesAsh tuff- 1-3% sulphides + minor gnt's''''Ash tuff- 1-3% sulphides + gnt's''Ash tuff- 1-3% sulphides + black mineral''Sulphidic ash- 5-10% sulphides''''''''''''''''

315.2 317 Ash tuff 3-5% disseminated, medium grained yellow sulphides.

Foliation & elongated sulphides (316m) 53

Page 2 of 3

NA18-03



327.2 335.8 Ash tuff 5-10% disseminated, medium grained yellow sulphides.

Foliation & elongated sulphides (328m) 52

335.8 339.3 Felsic Crystal TuffFoliated, pale grey quartz-eye crystal ash. Clasts, 5-10mm, at bottom contact. Look like sedimentary rip-up clasts deposited in thin bed.

Mineral elongation (339m) 50 522071 335.5 337 1.5 Light grey, siliceous ash- trace sulphides

339.3 454 Felsic Intrusive with minor volcanics

339.3 344.5 Spade Lake PorphrySame as previous porphyry unit but phenocrysts have a distinct 'popcorn' texture.

344.5 346 Ash tuff- Fine grained pale grey ash. 522195 344.8 345.8 1 1-3% disseminated, sulphides and QV in pale ash. Between SLP

346 363 Spade Lake Porphry363 365 Red Spade Lake Porphy

Red intrusive rock. Crystals are more tightly packed together, compared to porphry shallower in hole.

365 372 Spade Lake Porphry 1

372 375 Red Spade Lake Porphy375 403.5 Spade Lake Porphry 522194 389.3 390 0.7 QV with sulphides in SLP

403.5 411.3 Ash tuff- Pale pink, very fine-grained siliceous bands from 403.5 to 404. Foliated, light and dark grey bands. 522141522142522143522144522145522146522147522148522149

403.5404405406407407.5408409410

404405406407407.5408409410411

0.51110.50.5111

Felsic colour banding with trace sulphidesAsh tuff- 1-3% sulphides''''Ash tuff- 3-5% sulphides, sample taken from 407 to 408m with QV sample taken out of middle (522146)QV with trace sulphidesAsh tuff- 1-3% sulphides''Ash tufftrace sulphides

404 410 Ash tuff 1-3% disseminated sulphides.

411.3 414.5 Red Spade Lake Porphy414.5 418 Volcaniclastic Sediments- Very fine-grained, banded black sediments. Nil sulphides

418 454 Red Spade Lake Porphy

454 EOH

Page 3 of 3

APPENDIX C

CROSS SECTIONS

100

Overbuden

Interbedded amph metabasalt and tuffs


Biotite-rich crystal tuffInterbedded amph metabasalt and tuffs

Lapilli crystal tuff


200

Ash tuff

Mafic volcaniclastic sediments


Amph metabasalt

Amph metabasalt

Ash tuffCrystal tuffAmph metabasalt

Porphyritic/phenocrystic

Fe-carbonate rich unit (?)

Felsic ash with blue quartz

Colour banded tuff

Colour banded tuffIntermediate volcanic

banded flows

300

400

Overburden

100

Basalt Tuff

Felsic Tuff

Road Zone Trench

-100mRL

5,482,400mN

5,482,300mN

5,482,500mN

100mRL

0mRL

200mRL

300mRL

100mRL

200mRL

0mRL

-100mRL

5,482,000mN

5,482,100mN

5,482,200mN

261-

87-4

NA18-01

263178247651

North Abitibi Fall 2018 Drill ProgramDiamond Drill Hole Section

Line: 576300Hole: NA18-01

Section view: 270°Envelope width: 100m

25 50

metres

100

Office:

Tri Origin Exploration Ltd

Author: M Ruhl

0

Drawing:

Date: 12/8/2018

Scale: 1:3000 Projection: Non-Earth (meters)

OverbudenCrystal tuffVolcaniclastic sediments

100

Banded flows

Crystal tuff

Volcaniclastic sediments and tuffs

Amphibole metabasalt

Lapilli Tuff

200

300

Lapilli Tuff

Interbedded banded flows

and garnet tuffsPink lapilli tuff

Colour banded tuff

Amphibole metabasaltVolcaniclastic sediments and tuffs

Porphyritic intermediate volcanic flows with

white and pink phenocrysts and

minor volcaniclastic interflow seds.

Quartzo-feldspathic veins

Qtz-rich pink felsic altered,

high sulphide mineralization

400

Fe-carbonate rich unit

Overbuden

FG volcaniclastic sediments

Fe-carbonate rich unitWell foliated fine grained lapilli tuff

Amphibole metabasalt

Volcaniclastic seds

100

200

5,482,400mN

5,482,500mN

-100mRL

200mRL

0mRL

100mRL

300mRL

100mRL

200mRL

0mRL

5,482,300mN

-100mRL

5,482,100mN

5,482,200mN

NA-07-0

2

NA18-02

139496 161926




25 50

metres

100

Office:


Author: M Ruhl

0

Drawing:

Date: 12/8/2018


Amphibole metabasalt and minor volcaniclastic sediments


Finely laminated sediments

White feldspar crystal tuff


White feldspar crystal tuff

Finely laminated sediments

Overbuden

Interbedded white feldspar xl tuff and ash tuff

Sheared tuffaceous sediments

200

Felsic pink, blue quartz-rich crystal tuff

Interbedded ash and garnet tuffs

Sheared tuffaceous sediments

100



Overburden

300

Felsic crystal tuff

Black sedimentsRed Spade Lake Porphyry

Biotite-qrtz-fsp schist/

Seds

100

Feldspar quartz crystal tuff


Ash tuffs

400

Fine-grained biotite-quartz-feldspar schist /

Metawackes

Porphyritic flows / C

rystal tuffs

Ash tuffs



Seds


Seds


Seds

100

Spade Lake Porphyry

Overburden

Lapilli tuffs/Qtz-

fsp schist/Seds

5,483,500mN

5,483,600mN

0mRL

100mRL

200mRL

300mRL

100mRL

200mRL

0mRL

-100mRL-100mRL

5,483,400mN

5,483,100mN

5,483,200mN

5,483,300mN

NA18-03

BUR-43

BUR-12

BUR-14

193008193008




25 50

metres

100

Office:


Author: M Ruhl

0

Drawing:

Date: 12/8/2018


APPENDIX D

GEOCHEMICAL CERTIFICATES OF ANALYSIS

APPENDIX E

GEOCHEMICAL RESULTS

NA18-01 Appendix E:Au assay and trace element results

Analyte_unit_detection limit

Hole ID Fromm

Tom

Lengthm

SampleNo

Au_ppb_5

Ag_ppm_0.02

Al_pct_0.01

Ba_ppm_1

Ca_pct_0.01

Cr_ppm_1

Cu_ppm_0.5

Fe_pct_0.01

K_pct_0.01

Li_ppm_1

Mg_pct_0.01

Mn_ppm_2

Na_pct_0.01

Ni_ppm_0.5

P_ppm_100

S_pct_0.01

Sr_ppm_0.5

Ti_pct_0.01

V_ppm_2

Zn_ppm_1

Zr_ppm_0.5

As_ppm_1

Be_ppm_0.1

Bi_ppm_0.04

Cd_ppm_0.02

Ce_ppm_0.05

NA18-01 137 137.3 0.3 522044 55NA18-01 157.1 157.3 0.2 522045 5NA18-01 212 213 1 522046 161NA18-01 213 214 1 522047 7NA18-01 214 215 1 522048 13NA18-01 215 216 1 522049 52NA18-01 216 217 1 522050 16NA18-01 222 223 1 522210 7NA18-01 223 224 1 522211 8NA18-01 244 245 1 522051 39NA18-01 251 253 2 522052 7 0.38 8.07 737 4.66 123 72.2 7.8 1.55 244 1.86 1409 0.62 67.6 1230 0.15 318 0.84 225 182 36.3 <1 1.3 <0.04 0.29 26.79NA18-01 278.5 279 0.5 522053 10NA18-01 330 331 1 522025 -5 0.32 8.19 218 3.69 118 51.3 8.51 1.04 77 4.74 897 1.44 65.5 1278 0.02 229 0.83 207 59 43.2 1 0.6 <0.04 <0.02 28.76NA18-01 331 332 1 522026 -5 0.3 8.24 308 4.26 104 27.8 8.4 1.27 75 4.32 846 1.2 58.8 1533 0.03 312 0.9 201 41 44.9 2 0.7 <0.04 0.09 34.74NA18-01 332 333 1 522027 -5 0.12 7.99 263 5.2 83 15.8 8.76 1.18 66 3.8 862 0.86 58.5 1524 0.04 269 0.92 209 79 48.5 1 0.7 <0.04 0.1 36.62NA18-01 333 334 1 522028 7 0.26 8.66 350 4.64 102 65 10.3 0.97 61 1.89 1793 0.78 65.3 1569 0.04 263 0.97 237 75 49.4 1 0.8 <0.04 0.2 33.63NA18-01 334 335 1 522029 8 0.25 9.04 410 2.01 51 35.5 3.89 1.15 48 0.62 1109 1.62 46.4 1013 0.27 416 0.39 85 30 107 2 1 0.12 0.11 50.94NA18-01 335 336 1 522030 7 0.18 8.98 395 2.66 62 23.7 3.96 1.18 68 0.72 953 1.53 52.7 953 0.19 407 0.4 87 37 106 1 1.2 0.1 0.15 49.41NA18-01 336 337 1 522031 7 0.29 9.18 431 2.36 63 30.5 4.37 1.47 68 0.75 951 1.45 56.4 1009 0.25 413 0.4 88 76 107 <1 1.2 0.16 0.41 52.45NA18-01 337 338 1 522032 6 0.24 8.88 417 2.53 59 21.4 3.86 1.46 38 0.76 864 1.47 49.6 944 0.19 469 0.38 84 50 102 1 1.2 0.31 0.2 48.98NA18-01 338 339 1 522033 120 0.65 9.83 581 2.48 81 25.3 4.01 2.19 45 0.72 873 1.5 50.1 1107 0.36 585 0.45 107 80 120 2 1.5 0.43 0.4 51.53NA18-01 339 339.5 0.5 522034 97 0.81 9.52 615 2.57 51 18.8 3.48 2.06 29 0.66 755 1.95 45.5 991 0.54 689 0.39 88 68 106 1 1.9 0.49 0.33 54.57NA18-01 339.5 340 0.5 522035 454 1.55 9.29 687 2.92 64 13.8 4.49 1.9 72 0.91 979 1.29 55.4 1003 1.67 535 0.41 122 78 114 2 1.6 0.79 0.35 48.07NA18-01 340 341 1 522036 274 1.36 10.3 785 2.2 56 30.7 3.65 1.82 155 0.58 686 1.92 79.8 1251 1.26 846 0.35 94 63 108 1 1.8 0.81 0.09 74.3NA18-01 341 342 1 522037 117 0.83 8.99 650 2.39 88 30.7 3.29 1.46 93 0.51 631 1.83 71.3 1129 0.51 840 0.34 75 60 103 <1 1.7 0.51 0.12 67.16NA18-01 342 343 1 522038 42 0.47 8.29 720 4.25 130 24.4 3.8 1.78 44 1.31 711 2.26 115 1278 0.29 600 0.33 81 70 99.3 <1 1.4 0.08 0.22 64.45NA18-01 343 344 1 522039 1450 6.18 10.2 861 7.04 196 10 4.97 2.46 86 1.83 1035 2.42 162 1643 2.02 495 0.28 103 84 121 <1 1 0.37 0.12 101NA18-01 344 345 1 522040 216 0.94 10.7 708 6.72 173 6.6 3.85 2.29 80 1.76 737 3.14 133 1605 0.95 547 0.32 75 68 124 <1 1.1 0.13 0.1 83.14NA18-01 345 346 1 522041 10 0.22 8.23 440 3.36 100 27 3.62 1.44 46 0.91 506 2.82 115 1188 0.14 603 0.28 72 57 94 <1 1.2 0.05 0.09 60.39NA18-01 346 346.5 0.5 522042 159 0.39 7.88 470 4.93 79 16.6 3.78 1.28 36 1.32 976 2.62 118 1164 0.38 683 0.25 72 67 89.7 2 1.1 0.08 0.28 63.72NA18-01 346.5 347 0.5 522043 12 0.26 8.86 720 3.05 117 14.2 3.66 1.84 28 0.85 584 2.55 128 1303 0.16 831 0.3 79 59 102 1 1.7 0.07 0.18 64.24NA18-01 347 348 1 522054 7NA18-01 348 349 1 522055 12NA18-01 349 350 1 522056 7NA18-01 350 351 1 522057 15NA18-01 351 352 1 522058 5NA18-01 352 353 1 522059 8NA18-01 353 354 1 522060 7NA18-01 354 355 1 522061 6NA18-01 365 366 1 522062 234 0.44 10.7 803 1.82 55 11.1 2.47 2.58 30 0.5 446 3.11 45.2 1290 0.71 1069 0.32 76 57 92.5 1 1.7 0.16 0.08 71.31NA18-01 366 366.8 0.75 522063 83 0.57 4.04 366 0.81 36 1.2 2.24 1.27 18 0.24 238 0.6 71.6 542 1.84 441 0.1 33 25 36.6 2 0.9 0.3 0.08 73.14NA18-01 366.8 367.8 1 522064 8 0.34 8.3 1176 3.55 19 21.7 3.03 1.61 38 1.25 580 3.41 16.3 1571 0.34 1193 0.2 66 88 125 1 1.1 0.1 0.16 106NA18-01 390 391 1 522212 -5NA18-01 403 404 1 522213 -5NA18-01 404 405 1 522214 -5NA18-01 405 406 1 522215 -5NA18-01 416 417.4 1.4 522065 9 0.19 7.78 837 3.44 41 24 2.67 1.74 49 0.72 591 1.69 33.2 1126 0.59 1187 0.24 54 79 83.9 <1 1.3 0.12 0.2 68.9

Page 1 of 2



Hole ID Fromm

Tom

Lengthm

SampleNo

NA18-01 137 137.3 0.3 522044NA18-01 157.1 157.3 0.2 522045NA18-01 212 213 1 522046NA18-01 213 214 1 522047NA18-01 214 215 1 522048NA18-01 215 216 1 522049NA18-01 216 217 1 522050NA18-01 222 223 1 522210NA18-01 223 224 1 522211NA18-01 244 245 1 522051NA18-01 251 253 2 522052NA18-01 278.5 279 0.5 522053NA18-01 330 331 1 522025NA18-01 331 332 1 522026NA18-01 332 333 1 522027NA18-01 333 334 1 522028NA18-01 334 335 1 522029NA18-01 335 336 1 522030NA18-01 336 337 1 522031NA18-01 337 338 1 522032NA18-01 338 339 1 522033NA18-01 339 339.5 0.5 522034NA18-01 339.5 340 0.5 522035NA18-01 340 341 1 522036NA18-01 341 342 1 522037NA18-01 342 343 1 522038NA18-01 343 344 1 522039NA18-01 344 345 1 522040NA18-01 345 346 1 522041NA18-01 346 346.5 0.5 522042NA18-01 346.5 347 0.5 522043NA18-01 347 348 1 522054NA18-01 348 349 1 522055NA18-01 349 350 1 522056NA18-01 350 351 1 522057NA18-01 351 352 1 522058NA18-01 352 353 1 522059NA18-01 353 354 1 522060NA18-01 354 355 1 522061NA18-01 365 366 1 522062NA18-01 366 366.8 0.75 522063NA18-01 366.8 367.8 1 522064NA18-01 390 391 1 522212NA18-01 403 404 1 522213NA18-01 404 405 1 522214NA18-01 405 406 1 522215NA18-01 416 417.4 1.4 522065

Co_ppm_0.1

Cs_ppm_1

Ga_ppm_0.1

Hf_ppm_0.02

In_ppm_0.02

La_ppm_0.1

Lu_ppm_0.01

Mo_ppm_0.05

Nb_ppm_0.1

Pb_ppm_0.5

Rb_ppm_0.2

Sb_ppm_0.05

Sc_ppm_0.5

Se_ppm_2

Sn_ppm_0.3

Ta_ppm_0.05

Tb_ppm_0.05

Te_ppm_0.05

Th_ppm_0.2

Tl_ppm_0.02

U_ppm_0.05

W_ppm_0.1

Y_ppm_0.1

Yb_ppm_0.1

34.1 5 22 1.21 0.07 9.5 0.26 1.65 10.4 21.2 58 0.5 32.4 2 1.4 0.6 0.64 <0.05 0.5 0.69 0.15 3.7 23.8 1.9

40.5 4 20.1 2 0.06 10 0.39 0.49 10 6.7 32 0.66 31.9 <2 1.1 0.93 0.97 <0.05 0.4 0.28 0.1 0.1 26.2 339.5 4 20.6 1.57 0.06 11.7 0.4 0.29 11.3 9 40.2 0.72 32.5 <2 1 1.11 1.07 <0.05 0.4 0.42 0.12 <0.1 27.8 2.842.1 4 20 1.55 0.06 12.6 0.38 0.82 11 9.9 37.4 0.8 31.9 <2 1 0.95 1.06 <0.05 0.4 0.39 0.1 <0.1 27.9 2.9

43 6 23.3 1.78 0.07 11.9 0.34 1.86 10.7 11.6 35.8 0.74 35.6 <2 1 0.88 1.03 <0.05 0.5 0.26 0.16 0.3 25.1 2.519.5 2 22.1 3.26 0.04 22.2 0.18 0.89 5.2 19.8 34 0.84 12.5 <2 1.3 0.52 0.61 <0.05 2.8 0.44 0.72 0.4 12.7 1.318.9 3 22.5 3.27 0.04 21.4 0.2 0.9 5.4 17.9 36.8 0.63 13.4 <2 1 0.57 0.61 <0.05 2.5 0.45 0.68 0.6 13.2 1.420.7 4 23.2 3.21 0.03 22.9 0.19 0.82 5 53.4 47.1 0.68 12.5 <2 1.8 0.49 0.63 <0.05 2.9 0.56 0.74 1.1 13.5 1.316.9 5 22.3 3.11 0.03 21.6 0.19 0.77 5 21 45.9 0.71 12.6 <2 0.9 0.53 0.58 <0.05 2.6 0.56 0.7 2.2 12.9 1.319.3 6 25.1 3.61 0.04 22.7 0.22 1.14 6 35.7 64.8 0.6 15.5 <2 1.4 0.6 0.62 0.25 2.6 0.84 0.81 6 13.4 1.419.7 8 24.6 3.18 0.04 23.5 0.17 0.62 4.6 41.3 63.9 0.62 12.7 <2 0.9 0.52 0.74 0.25 3.1 0.84 0.8 8.1 12.6 1.221.6 10 28.6 3.82 0.05 21.1 0.18 6.64 6 38.2 82.7 0.76 13.2 <2 1.1 0.52 0.42 0.83 2.7 1.08 0.85 10.3 11.7 1.122.9 5 29 4.03 0.05 33.2 0.16 3.31 5.5 37.6 59.7 0.67 10.4 <2 1.2 0.59 0.5 0.7 4.7 0.67 1.21 8.7 11.2 118.7 5 24.4 3.78 0.03 30.4 0.13 1.94 4.5 33.8 48.4 0.76 9.2 <2 1 0.44 0.47 0.37 4.3 0.61 1.19 8.3 11.3 0.921.1 7 23.1 3.53 0.04 28.4 0.11 1.16 2.9 22.6 60.6 0.75 10.3 <2 1 0.32 0.4 0.12 4 0.73 1.04 6.2 9.5 0.837.3 6 30.4 4.41 0.08 45 0.17 1.44 3 17.2 87.2 1.01 13.2 <2 1 0.57 0.6 2.71 5 1.01 1.17 17.5 15.7 1.123.7 6 29.3 4.38 0.05 36.2 0.15 0.69 1.9 15.6 77.4 0.87 12.9 <2 0.9 0.27 0.54 0.44 5 0.88 1.2 14.5 13.4 119.2 4 23.2 3.38 0.03 26.5 0.11 0.76 2.2 13.5 45.6 0.71 9.8 <2 0.8 0.18 0.39 0.07 3.8 0.56 1 3.7 9.6 0.723.1 4 22 3.23 0.04 28.1 0.12 0.88 1.7 20.2 41.3 0.48 9.6 <2 0.8 0.15 0.43 0.21 3.7 0.51 0.92 3.3 10.2 0.920.5 5 23.5 3.09 0.03 28.2 0.11 0.75 2.7 21.9 54.3 0.64 10.6 <2 0.7 0.32 0.49 0.06 4 0.66 1.09 4.2 9.4 0.9

12.7 8 29.9 2.84 0.04 32 0.1 1.66 4.3 33.7 73.4 0.78 9.2 <2 0.9 0.52 0.39 0.25 4.7 0.98 1.21 7.1 8.8 0.632.6 3 11 1.05 0.02 34 0.04 1.19 0.6 16.4 33.9 0.41 3.5 <2 0.6 <0.05 0.31 0.41 3.1 0.42 0.46 2.4 4.8 0.311.4 8 22 3.31 0.03 49.6 0.1 1.92 2.4 19 52.6 0.58 7.7 <2 2.7 0.27 0.41 0.14 3.9 0.74 0.79 1.7 9.1 0.6

11.2 7 21.1 2.25 0.03 31.8 0.07 1.76 2.1 22 54.6 0.74 6.7 <2 0.9 0.13 0.35 0.07 3.4 0.77 0.86 1.1 8 0.5

Page 2 of 2



Hole ID Fromm

Tom

Lengthm

SampleNo

Au_ppb_5

Ag_ppm_0.02

Al_pct_0.01

Ba_ppm_1 Ca_pct_0.01

Cr_ppm_1

Cu_ppm_0.5

Fe_pct_0.01

K_pct_0.01

Li_ppm_1

Mg_pct_0.01

Mn_ppm_2

Na_pct_0.01

Ni_ppm_0.5

P_ppm_100

S_pct_0.01

Sr_ppm_0.5

Ti_pct_0.01

V_ppm_2

Zn_ppm_1

Zr_ppm_0.5

As_ppm_1

Be_ppm_0.1

Bi_ppm_0.04

NA18-02 39 39.5 0.5 522165 6NA18-02 39.5 40.5 1 522166 -5NA18-02 40.5 41.5 1 522167 5NA18-02 41.5 42.5 1 522168 -5NA18-02 42.5 43 0.5 522169 -5NA18-02 43 44 1 522170 -5NA18-02 85 86 1 522171 7NA18-02 86 87 1 522172 12NA18-02 87 88 1 522173 -5NA18-02 88 89 1 522174 -5NA18-02 89 90 1 522175 -5NA18-02 164 165 1 522176 49NA18-02 195.7 196.2 0.5 522177 28NA18-02 198 199 1 522178 6NA18-02 199 200 1 522179 52NA18-02 200 201 1 522180 769NA18-02 274 275 1 522181 -5NA18-02 275 276 1 522182 272NA18-02 276 277 1 522183 11NA18-02 277 278 1 522184 7NA18-02 278 279 1 522185 1505 1.09 8.54 709 1.76 43 61.1 3.96 2.34 84 0.86 1119 1.09 40.4 1102 0.9 480 0.34 79 43 104 <1 1.1 0.36NA18-02 279 280 1 522186 97 0.54 8.48 651 2.56 45 31.3 3.54 1.94 81 0.94 958 1.17 37.6 1119 0.34 522 0.34 76 58 105 <1 1.7 0.27NA18-02 280 280.5 0.5 522187 2354 5.46 7.62 258 1.7 40 14.4 4.78 1.85 58 0.64 659 1.26 44.5 946 3.05 410 0.27 82 21 89.6 1 1.5 0.89NA18-02 280.5 281.5 1 522188 55 0.39 8.55 595 1.77 38 27.2 3.61 2.31 47 0.82 741 1.16 42.3 1097 0.19 484 0.33 77 76 101 <1 1.5 0.25NA18-02 281.5 282.5 1 522189 43 0.46 8.33 542 2.38 41 20.9 3.43 2.11 42 0.78 761 1.27 38.6 1100 0.45 561 0.33 76 58 97.5 <1 1.6 0.41NA18-02 282.5 283 0.5 522190 599 1.12 7.73 727 1.69 36 6.6 2.7 2.6 49 0.51 708 0.91 28 959 1.09 400 0.29 88 25 89.8 <1 1.2 0.37NA18-02 283 284 1 522191 1408 4.11 8.13 561 2.72 46 44.9 3.23 2.28 65 0.65 925 1.58 29.8 929 1.66 426 0.28 78 29 94.8 <1 1.9 0.26NA18-02 284 285 1 522192 1668 4.91 7.68 169 3.15 40 29.3 6.09 1.73 50 0.64 1235 1.6 49.4 900 3.9 423 0.34 98 71 90.3 <1 1.7 0.57NA18-02 285 286 1 522193 79 1.79 8.34 676 2.63 64 25.9 3.9 1.56 46 0.67 1797 1.3 38.7 826 0.38 382 0.42 113 286 95.7 <1 1.3 0.14NA18-02 316 317 1 522204 -5NA18-02 317 318 1 522205 9NA18-02 322.5 323.5 1 522203 12NA18-02 334.5 335.5 1 522206 16NA18-02 335.5 336.5 1 522207 8NA18-02 336.5 337.5 1 522208 40NA18-02 337.5 339 1.5 522209 23

Page 1 of 2



Hole ID Fromm

Tom

Lengthm

SampleNo

NA18-02 39 39.5 0.5 522165NA18-02 39.5 40.5 1 522166NA18-02 40.5 41.5 1 522167NA18-02 41.5 42.5 1 522168NA18-02 42.5 43 0.5 522169NA18-02 43 44 1 522170NA18-02 85 86 1 522171NA18-02 86 87 1 522172NA18-02 87 88 1 522173NA18-02 88 89 1 522174NA18-02 89 90 1 522175NA18-02 164 165 1 522176NA18-02 195.7 196.2 0.5 522177NA18-02 198 199 1 522178NA18-02 199 200 1 522179NA18-02 200 201 1 522180NA18-02 274 275 1 522181NA18-02 275 276 1 522182NA18-02 276 277 1 522183NA18-02 277 278 1 522184NA18-02 278 279 1 522185NA18-02 279 280 1 522186NA18-02 280 280.5 0.5 522187NA18-02 280.5 281.5 1 522188NA18-02 281.5 282.5 1 522189NA18-02 282.5 283 0.5 522190NA18-02 283 284 1 522191NA18-02 284 285 1 522192NA18-02 285 286 1 522193NA18-02 316 317 1 522204NA18-02 317 318 1 522205NA18-02 322.5 323.5 1 522203NA18-02 334.5 335.5 1 522206NA18-02 335.5 336.5 1 522207NA18-02 336.5 337.5 1 522208NA18-02 337.5 339 1.5 522209

Cd_ppm_0.02

Ce_ppm_0.05

Co_ppm_0.1

Cs_ppm_1

Ga_ppm_0.1

Hf_ppm_0.02

In_ppm_0.02

La_ppm_0.1

Lu_ppm_0.01

Mo_ppm_0.05

Nb_ppm_0.1

Pb_ppm_0.5

Rb_ppm_0.2

Sb_ppm_0.05

Sc_ppm_0.5

Se_ppm_2

Sn_ppm_0.3

Ta_ppm_0.05

Tb_ppm_0.05

Te_ppm_0.05

Th_ppm_0.2

Tl_ppm_0.02

U_ppm_0.05

W_ppm_0.1

Y_ppm_0.1

Yb_ppm_0.1

0.18 59.69 23.4 9 24.2 3.01 0.03 26.3 0.14 7.84 6.7 19.7 79.2 0.73 10.2 <2 3.4 0.89 0.42 0.14 3.9 0.89 0.92 4.8 10.1 0.90.16 62.74 16.7 9 23.8 2.88 0.04 28.3 0.15 1.84 5.5 22.7 69 0.71 11.1 <2 1 0.69 0.46 0.2 3.5 0.82 0.86 7.1 11.3 10.1 47.76 34.9 5 19.7 2.55 0.05 21.3 0.12 4.36 4 19.1 57.5 0.57 9.7 <2 1.1 0.5 0.37 2.72 3.2 0.6 0.72 10.4 8.5 0.7

0.12 59.54 16.4 7 24.8 2.86 0.04 26.3 0.14 0.65 4.6 25.9 80.3 0.44 11.2 <2 1 0.45 0.44 0.21 3.6 0.96 0.93 5.2 10.9 10.17 60.15 17.2 7 23.8 2.8 0.03 26.8 0.14 0.91 4.8 29.4 77.7 0.53 11 <2 1 0.59 0.44 0.26 3.5 1 0.86 6.5 11 0.90.07 54.63 18 6 22.4 2.56 0.05 24.5 0.11 1.91 3.5 22 83.2 0.44 10.1 <2 1.1 0.31 0.38 0.63 3.3 0.94 0.72 11.4 9.2 0.80.18 66.8 12.1 6 22 2.67 0.06 30.8 0.13 1.94 3.4 22.7 78.7 0.45 10.5 <2 1 0.47 0.47 1.97 2.9 0.84 0.61 16.2 10.9 0.90.45 43.06 20.5 6 20.7 2.5 0.07 18.4 0.16 0.74 4.3 32.2 57.8 0.49 12.4 <2 1 0.49 0.47 2.25 2.7 0.64 0.57 25.4 12 1.11.79 40.52 15.4 6 22.6 2.67 0.05 17.7 0.19 1.03 5.5 161 56.6 1.14 16.9 <2 1.1 0.51 0.48 0.3 2.2 0.71 0.54 6.9 13.2 1.2

Page 2 of 2



Hole ID Fromm

Tom

Lengthm

SampleNo

Au_ppb_5

Ag_ppm_0.02

Al_pct_0.01

Ba_ppm_1

Ca_pct_0.01

Cr_ppm_1

Cu_ppm_0.5

Fe_pct_0.01

K_pct_0.01

Li_ppm_1

Mg_pct_0.01

Mn_ppm_2

Na_pct_0.01

Ni_ppm_0.5

P_ppm_100

S_pct_0.01

Sr_ppm_0.5

Ti_pct_0.01

V_ppm_2

Zn_ppm_1

Zr_ppm_0.5

As_ppm_1

Be_ppm_0.1

Bi_ppm_0.04

Cd_ppm_0.02

NA18-03 60.6 61 0.4 522150 10 1.05 6.68 203 1.2 87 116 7.3 1.76 28 1.09 390 1.52 31.1 464 >5 115 0.15 52 164 92.7 <1 0.4 0.32 0.18NA18-03 79 80 1 522151 8 1.75 8.69 163 5.3 143 72.4 6.8 1.89 25 2.06 1362 1.57 39.5 831 0.94 181 0.6 160 240 68.2 <1 0.7 0.1 0.61NA18-03 80 81 1 522152 14 3.1 8.25 240 4.14 97 90.5 5.04 2.17 25 1.44 740 1.7 33.6 650 1.48 136 0.33 84 306 107 <1 0.5 0.16 1.02NA18-03 81 82 1 522153 8 1.13 8.46 213 3.06 76 62 5.27 1.91 26 2.37 690 1.79 43 751 0.78 173 0.38 116 71 97.1 <1 0.7 0.08 0.09NA18-03 82 83 1 522154 6 0.84 8.61 262 2.24 57 43.5 4.96 1.95 27 1.93 574 2.05 37.7 720 1 184 0.34 96 46 109 <1 0.9 0.08 0.07NA18-03 109 110.2 1.2 522155 9 0.97 8.75 593 2.53 32 6.2 2.06 1.17 30 0.9 344 3.96 21.5 790 1.15 516 0.18 49 57 69.6 2 1.2 0.27 0.11NA18-03 110.2 111 0.8 522156 7 0.43 7.86 162 5.5 70 67.9 8.34 0.86 29 2.9 1454 1.87 25.5 977 0.48 347 0.87 262 140 29.7 1 0.7 0.09 0.16NA18-03 111 112 1 522157 7 0.32 7.98 164 5.15 105 90.6 9.18 1.14 42 3.24 1472 1.91 26 1079 0.26 286 0.99 294 133 22.4 1 0.5 0.07 0.14NA18-03 112 113 1 522158 6 0.28 8.81 213 5.66 174 70.2 8.08 1.52 47 3.28 1429 2.13 40.7 1035 0.22 343 0.74 236 173 22.2 <1 0.9 0.09 0.16NA18-03 113 114 1 522159 7 0.18 8.7 729 2.79 32 4.8 1.97 1.42 26 0.87 294 3.84 19.9 742 1.14 622 0.14 47 46 73.8 1 1.4 0.12 0.03NA18-03 114 114.8 0.8 522160 6 0.14 8.81 711 2.95 40 7.7 2.03 1.55 28 0.95 360 3.49 23.8 711 1.2 666 0.15 50 55 64.9 1 1 0.13 0.09NA18-03 114.8 116 1.2 522161 12 0.33 8.61 38 5.95 226 62 8.32 0.54 26 4.37 1478 1.8 124 673 0.37 247 0.61 196 186 7 <1 0.5 0.09 0.24NA18-03 116 117 1 522162 10 0.41 8.85 31 5.41 192 61.5 8.52 0.46 26 4.22 1577 1.95 104 803 0.09 279 0.68 213 206 11.8 <1 0.3 0.06 0.24NA18-03 117 118 1 522163 7 0.39 7.84 41 5.37 85 74.3 8.19 0.45 19 2.85 1535 2.22 41.2 1178 0.2 269 0.76 223 163 16.2 <1 0.6 0.18 0.28NA18-03 118 119 1 522164 10 0.68 7.97 249 4.93 78 112 6.94 1.63 31 1.86 1209 2.13 37.4 994 0.96 299 0.62 181 150 38.5 2 0.5 0.36 0.19NA18-03 225 226 1 522198 28NA18-03 226 227 1 522199 98NA18-03 227 228 1 522200 12NA18-03 228 229 1 522201 16NA18-03 229 230 1 522202 24NA18-03 232.5 233.5 1 522076 49NA18-03 239 240 1 522077 117NA18-03 240 241 1 522078 113NA18-03 241 242 1 522079 68NA18-03 242 243 1 522080 62NA18-03 243 244 1 522081 81NA18-03 244 245 1 522082 150NA18-03 245 246 1 522083 110 0.79 8.66 173 0.54 32 88.1 4.46 3.75 19 0.63 531 0.3 21.4 960 3.4 173 0.18 56 79 87.6 3 0.9 7.46 0.05NA18-03 246 247 1 522084 135 6.89 7.59 77 0.68 27 562 6.19 3.21 23 0.84 940 0.23 21.6 917 4.23 161 0.32 66 180 127 3 0.9 10 0.21NA18-03 247 248 1 522085 351 4.33 7.79 45 0.61 44 224 7.42 3.25 16 0.39 546 0.27 39.2 873 >5 164 0.15 52 77 74.7 3 1.1 8.89 0.14NA18-03 248 249 1 522086 60 0.77 8.82 354 0.49 31 60.3 3.63 3.54 15 0.47 323 0.29 18.8 866 3.42 234 0.14 52 57 89.2 3 1 2.55 0.06NA18-03 249 250 1 522087 173NA18-03 250 251 1 522088 142NA18-03 251 252 1 522089 127NA18-03 252 253 1 522090 213NA18-03 253 254 1 522091 208 1.2 6.77 80 0.65 58 327 7.2 2.09 23 1.56 1070 0.33 43.6 927 3.96 111 0.37 103 245 102 2 0.8 1.25 0.31NA18-03 254 255 1 522092 212 0.88 7.45 65 0.43 35 261 7.62 2.58 20 1.09 585 0.31 37.1 1060 >5 117 0.21 78 139 105 2 0.9 3.1 0.51NA18-03 255 256 1 522093 119 1.67 7.98 76 0.56 49 393 7.39 2.65 24 1.37 753 0.46 44.4 842 >5 186 0.25 73 211 77.4 <1 1.1 3.47 0.16NA18-03 256 257 1 522094 96 2.35 7.81 66 0.76 46 530 6.24 2.76 24 1.38 1003 0.45 45.1 1117 4.46 182 0.31 97 392 91.2 2 0.9 5.49 2.27NA18-03 257 258 1 522095 121 1.95 8.19 103 1.17 64 969 7.6 2.14 34 2.47 1546 0.59 46.1 1220 3.27 216 0.58 207 406 99 1 0.7 2.99 0.51NA18-03 258 259 1 522096 124 2.58 7.74 79 1.24 79 919 8.61 1.85 40 2.95 1473 0.52 52.9 1253 4.28 274 0.64 238 484 106 1 0.7 3.2 0.45NA18-03 259 260 1 522097 173NA18-03 260 261 1 522098 132NA18-03 261 262 1 522099 161NA18-03 262 263 1 522100 204NA18-03 263 264 1 522101 169NA18-03 264 265 1 522102 215NA18-03 265 266 1 522103 109NA18-03 266 267 1 522104 160NA18-03 267 268 1 522105 174NA18-03 268 269 1 522106 120NA18-03 269 270 1 522107 179NA18-03 270 271 1 522108 228NA18-03 271 272 1 522109 135NA18-03 272 273 1 522110 119

Page 1 of 4



Hole ID Fromm

Tom

Lengthm

SampleNo

NA18-03 60.6 61 0.4 522150NA18-03 79 80 1 522151NA18-03 80 81 1 522152NA18-03 81 82 1 522153NA18-03 82 83 1 522154NA18-03 109 110.2 1.2 522155NA18-03 110.2 111 0.8 522156NA18-03 111 112 1 522157NA18-03 112 113 1 522158NA18-03 113 114 1 522159NA18-03 114 114.8 0.8 522160NA18-03 114.8 116 1.2 522161NA18-03 116 117 1 522162NA18-03 117 118 1 522163NA18-03 118 119 1 522164NA18-03 225 226 1 522198NA18-03 226 227 1 522199NA18-03 227 228 1 522200NA18-03 228 229 1 522201NA18-03 229 230 1 522202NA18-03 232.5 233.5 1 522076NA18-03 239 240 1 522077NA18-03 240 241 1 522078NA18-03 241 242 1 522079NA18-03 242 243 1 522080NA18-03 243 244 1 522081NA18-03 244 245 1 522082NA18-03 245 246 1 522083NA18-03 246 247 1 522084NA18-03 247 248 1 522085NA18-03 248 249 1 522086NA18-03 249 250 1 522087NA18-03 250 251 1 522088NA18-03 251 252 1 522089NA18-03 252 253 1 522090NA18-03 253 254 1 522091NA18-03 254 255 1 522092NA18-03 255 256 1 522093NA18-03 256 257 1 522094NA18-03 257 258 1 522095NA18-03 258 259 1 522096NA18-03 259 260 1 522097NA18-03 260 261 1 522098NA18-03 261 262 1 522099NA18-03 262 263 1 522100NA18-03 263 264 1 522101NA18-03 264 265 1 522102NA18-03 265 266 1 522103NA18-03 266 267 1 522104NA18-03 267 268 1 522105NA18-03 268 269 1 522106NA18-03 269 270 1 522107NA18-03 270 271 1 522108NA18-03 271 272 1 522109NA18-03 272 273 1 522110

Ce_ppm_0.05

Co_ppm_0.1

Cs_ppm_1

Ga_ppm_0.1

Hf_ppm_0.02

In_ppm_0.02

La_ppm_0.1

Lu_ppm_0.01

Mo_ppm_0.05

Nb_ppm_0.1

Pb_ppm_0.5

Rb_ppm_0.2

Sb_ppm_0.05

Sc_ppm_0.5

Se_ppm_2

Sn_ppm_0.3

Ta_ppm_0.05

Tb_ppm_0.05

Te_ppm_0.05

Th_ppm_0.2

Tl_ppm_0.02

U_ppm_0.05

W_ppm_0.1

Y_ppm_0.1

Yb_ppm_0.1

31.33 83.1 1 14.9 2.38 0.05 13.8 0.17 3.9 2.3 8.9 49.4 0.13 7.6 2 1.2 0.2 0.38 0.5 1.5 0.31 0.52 0.8 11.5 1.122.21 31.5 1 18.6 1.84 0.09 8.7 0.36 2.14 6.7 12.7 40.3 0.11 25.6 <2 1.3 0.61 0.68 0.16 0.8 0.25 0.22 0.5 23.4 2.325.34 28.7 2 18.1 2.7 0.07 10.6 0.25 3.28 5.2 10.7 46.3 0.11 14.2 <2 1.5 0.51 0.5 0.33 1.4 0.3 0.4 0.5 15.6 1.627.19 23.4 2 17.9 2.51 0.04 11.7 0.23 2.38 5.1 9 43.8 0.09 16 <2 1.2 0.62 0.42 0.2 1.3 0.26 0.37 0.4 13.7 1.430.98 19.4 2 18.4 2.9 0.04 13.3 0.18 1.51 5.3 8.2 45.3 0.08 13 <2 1 0.55 0.4 0.16 1.5 0.22 0.4 0.3 10.6 1.156.47 9.3 1 19.9 2.06 0.02 26.1 0.1 1.78 1.9 12 30.4 0.08 6.4 <2 0.5 0.15 0.36 0.66 4.5 0.19 1.3 0.3 8.8 0.723.73 33.4 2 19.1 0.84 0.08 9 0.5 1.42 6.6 11.8 23.8 0.28 35.2 <2 0.8 0.51 0.88 0.22 1 0.18 0.28 0.3 32.7 3.320.46 39.9 5 19.4 0.66 0.09 7.1 0.58 0.94 8.3 9.5 40.4 0.3 40.7 <2 1 0.8 0.97 0.1 0.5 0.36 0.15 0.3 37 3.722.44 33.8 7 17.4 0.71 0.07 8.8 0.41 0.81 6.6 11 53.5 0.17 32.5 <2 1 0.68 0.73 0.1 0.6 0.47 0.18 0.3 26.4 2.757.3 8.5 2 21.8 2.12 0.02 27 0.1 1.37 1.7 8.9 38 0.08 5.5 <2 0.6 0.2 0.32 0.18 4.5 0.28 1.24 0.3 7.3 0.6

53.79 9.3 2 20.3 1.88 0.03 25.2 0.1 1.53 1.3 10.6 45.2 0.05 5.6 <2 0.6 0.1 0.34 0.18 4.2 0.31 1.23 0.3 7.4 0.612.77 48.1 <1 16.5 0.29 0.07 4.6 0.34 0.72 5.1 12.4 12 0.26 27 <2 0.9 0.57 0.61 0.15 0.3 0.12 0.14 0.3 22.5 2.315.92 45.1 <1 17.5 0.46 0.07 5.7 0.43 0.67 6.1 14.6 8.8 0.38 30.6 <2 1.1 0.65 0.71 0.07 0.4 0.09 0.11 0.3 26.9 2.823.86 32 <1 17 0.69 0.09 8.7 0.43 1.77 8.8 13.1 9 0.23 31.7 <2 1.1 0.7 0.85 0.11 0.5 0.09 0.13 0.3 31.4 325.25 28.7 2 17 1.33 0.11 10.2 0.35 1.87 8 12.8 42.6 0.16 24.5 <2 1.3 0.54 0.73 0.17 0.8 0.35 0.24 0.9 25.4 2.4

76.99 12 5 15.9 2.67 0.07 38.7 0.09 14.08 4.9 27.4 148 0.38 5.6 <2 1.2 0.71 0.3 3.53 4.8 1.51 1.23 5.4 7.5 0.666.23 15.4 7 20.2 3.17 0.18 31.6 0.22 11.28 6.3 25.9 137 0.26 9.2 2 1.7 0.59 0.57 3.17 3.6 1.51 1.69 10.3 16.9 1.368.55 17.8 3 15.9 2.17 0.15 32 0.08 36.66 2.2 26.3 119 0.31 5.3 4 1.6 0.34 0.33 5.01 4.2 1.12 1.25 6 7.1 0.588.6 8.8 3 11.8 2.47 0.05 45.5 0.08 8.61 2.3 31.5 133 0.24 5.2 <2 1 0.4 0.32 1.05 4.5 1.19 1.16 4.7 7.3 0.6

34.47 31.4 4 15.8 2.63 0.08 15 0.19 10.6 5.3 23 89.8 0.34 13.5 4 2.7 0.56 0.43 0.93 2.4 0.89 0.79 6 13.6 1.249.66 37.3 3 15.8 2.68 0.09 21.8 0.13 9.6 3 29.3 106 0.33 8.9 5 2.5 0.31 0.37 1.52 3.8 0.99 0.96 3.6 9.3 0.842.78 28.7 5 18.2 2.16 0.14 19.2 0.1 4.5 3.1 42.4 115 0.34 8.6 4 2.4 0.35 0.32 1.27 3 1.26 0.79 4 8 0.756.45 31.6 6 19.3 2.38 0.22 24.9 0.16 10.54 4.6 65.1 118 0.41 11 4 2.7 0.55 0.44 1.7 3.7 1.3 1.09 4 11.7 142.35 29.8 6 20.1 2.46 0.22 18.1 0.3 12.65 6.4 37 94.8 0.53 25.5 4 3.3 0.66 0.61 1.12 1.8 1.06 0.82 6.6 19.7 1.937.42 34.3 7 19.2 2.76 0.23 15.2 0.37 18.07 6.2 28.3 87.5 0.42 29.8 4 3.7 0.69 0.7 1.18 1.1 1.04 0.98 4.7 23 2.3

Page 2 of 4



Hole ID Fromm

Tom

Lengthm

SampleNo

Au_ppb_5

Ag_ppm_0.02

Al_pct_0.01

Ba_ppm_1

Ca_pct_0.01

Cr_ppm_1

Cu_ppm_0.5

Fe_pct_0.01

K_pct_0.01

Li_ppm_1

Mg_pct_0.01

Mn_ppm_2

Na_pct_0.01

Ni_ppm_0.5

P_ppm_100

S_pct_0.01

Sr_ppm_0.5

Ti_pct_0.01

V_ppm_2

Zn_ppm_1

Zr_ppm_0.5

As_ppm_1

Be_ppm_0.1

Bi_ppm_0.04

Cd_ppm_0.02

NA18-03 273 274 1 522111 220NA18-03 274 275 1 522112 140NA18-03 275 276 1 522113 148 2.74 8.82 449 0.82 91 1975 3.61 2.95 32 1.09 1523 1.76 42.1 1025 1.01 299 0.27 72 348 65.8 3 1.4 0.49 1.37NA18-03 276 277 1 522114 149 1.7 7.91 450 1.05 101 2375 4.41 2.52 32 1.08 1356 1.71 41.8 1746 1.19 332 0.2 65 207 53.2 5 1.1 0.41 0.41NA18-03 277 278 1 522115 352 2.61 8.29 431 0.97 80 3512 5.29 3.03 33 1.23 1655 1.31 53.3 1994 1.55 278 0.32 92 317 66.8 5 1.4 0.41 0.76NA18-03 278 279 1 522116 167 1.9 9.09 340 0.67 96 1594 4.59 3.4 31 0.96 2246 1.4 48.2 1190 1.18 264 0.31 83 298 70.4 4 0.9 0.24 0.73NA18-03 279 280 1 522117 88NA18-03 280 281 1 522118 64NA18-03 281 282 1 522119 68NA18-03 282 283 1 522120 87NA18-03 283 284 1 522121 85NA18-03 284 285 1 522122 92NA18-03 285 286 1 522123 193NA18-03 286 287 1 522124 117NA18-03 287 288 1 522125 144 4.17 8.47 44 1.06 96 818 8.12 3.3 26 0.97 809 0.75 82.3 903 >5 216 0.52 143 787 98 13 1.1 3.03 3.06NA18-03 288 289 1 522126 134 3.38 8.02 48 1.05 116 967 7.92 3.1 27 0.96 756 0.91 78.8 733 >5 242 0.46 130 598 86.7 12 1.1 2.56 2.33NA18-03 289 290 1 522127 121NA18-03 290 291 1 522128 157NA18-03 291 292 1 522129 188NA18-03 292 292.5 0.5 522130 63NA18-03 294.8 295.8 1 522196 64 1.35 7.29 484 3.02 88 554 5.03 3.66 60 2.08 695 0.46 57.6 869 2.05 398 0.38 166 380 95.9 8 1.2 0.98 0.98NA18-03 295.8 296.2 0.4 522197 61 1.47 7.12 289 3.84 59 662 5.34 3.32 61 2.08 711 1.03 55.4 678 2.37 812 0.36 128 397 84.3 7 1.5 0.77 1.2NA18-03 315.2 316.2 1 522131 103NA18-03 316.2 317.2 1 522132 137NA18-03 318.6 319.6 1 522133 203NA18-03 319.6 321 1.4 522134 108NA18-03 321 322 1 522135 72NA18-03 322 323 1 522136 157NA18-03 323 324 1 522137 91NA18-03 324 325 1 522138 122NA18-03 325 326 1 522139 104NA18-03 326 327 1 522140 113NA18-03 327 328 1 522066 123 2.96 7.44 117 1.04 70 979 12 3.3 22 0.9 6121 0.2 83.4 1458 4.93 262 0.37 113 746 74 11 1.6 1.45 2NA18-03 328 329 1 522067 128 3.94 7.93 101 1.22 62 905 9.67 3.71 21 0.73 2739 0.25 82 929 >5 281 0.47 123 648 80.8 9 1.6 3.3 1.24NA18-03 329 330 1 522072 107 3.89 8.21 103 0.69 78 759 8.2 3.9 19 0.62 1838 0.22 75.8 967 4.87 227 0.48 128 574 90.3 11 1.7 2.59 1.34NA18-03 330 331 1 522073 140 2.94 8.16 103 0.65 82 1064 8.93 3.95 22 0.64 1248 0.24 89.5 933 >5 217 0.51 143 494 90.5 10 1.8 1.2 1.11NA18-03 331 332 1 522074 102 4.11 8.36 99 0.79 76 901 7.86 4.06 24 0.63 1747 0.27 80.5 887 4.82 236 0.5 139 433 92.9 9 1.6 2.63 0.99NA18-03 332 333 1 522075 125 4.08 7.33 107 0.89 83 999 7.73 3.66 25 0.72 1139 0.2 80.7 781 4.89 178 0.44 123 491 83.3 10 1.6 2.37 1.16NA18-03 333 334 1 522068 92 2.27 9.15 121 0.71 100 616 8.48 4.5 29 0.84 1126 0.21 87.5 950 4.74 187 0.6 157 339 105 13 2 1.78 0.67NA18-03 334 335 1 522069 70 2.18 7.99 242 0.52 84 821 5.43 3.86 25 0.59 753 0.18 53.7 689 3.23 168 0.44 104 216 107 9 1.8 0.79 0.59NA18-03 335 335.5 0.5 522070 99 6.29 6.28 111 0.78 40 2341 5.18 3.04 25 0.52 372 0.17 28.6 297 4.18 554 0.13 32 1753 89.1 5 1.1 2.62 7.66NA18-03 335.5 337 1.5 522071 70 0.83 6.72 779 0.21 10 671 1.31 3.29 15 0.27 90 0.12 10.2 107 0.6 194 0.06 10 617 136 2 1.5 0.28 2.6NA18-03 344.8 345.8 1 522195 432 1.47 7.59 690 1.38 82 254 3.98 4.12 40 1.22 435 0.34 60.1 723 1.61 215 0.31 108 129 94 3 1.3 0.34 0.07NA18-03 389.3 390 0.7 522194 7833NA18-03 403.5 404 0.5 522141 32 0.56 7.61 756 0.43 42 64.8 1.45 2.41 17 0.25 204 2.52 3.9 <100 0.63 367 0.03 5 96 119 <1 1.1 0.39 0.32NA18-03 404 405 1 522142 275 1.92 9.06 390 0.96 80 84.7 3.46 4.12 28 0.74 586 1.43 35.6 1662 2.35 204 0.22 48 176 108 2 1.7 1.45 0.45NA18-03 405 406 1 522143 125 3.94 9.29 771 1.29 72 122 2.3 3.62 26 0.73 510 1.68 21.1 974 1.15 368 0.19 40 175 79.7 <1 1.4 2.25 0.36NA18-03 406 407 1 522144 23NA18-03 407 407.5 0.5 522145 334NA18-03 407.5 408 0.5 522146 150NA18-03 408 409 1 522147 24NA18-03 409 410 1 522148 88NA18-03 410 411 1 522149 30

Page 3 of 4



Hole ID Fromm

Tom

Lengthm

SampleNo

NA18-03 273 274 1 522111NA18-03 274 275 1 522112NA18-03 275 276 1 522113NA18-03 276 277 1 522114NA18-03 277 278 1 522115NA18-03 278 279 1 522116NA18-03 279 280 1 522117NA18-03 280 281 1 522118NA18-03 281 282 1 522119NA18-03 282 283 1 522120NA18-03 283 284 1 522121NA18-03 284 285 1 522122NA18-03 285 286 1 522123NA18-03 286 287 1 522124NA18-03 287 288 1 522125NA18-03 288 289 1 522126NA18-03 289 290 1 522127NA18-03 290 291 1 522128NA18-03 291 292 1 522129NA18-03 292 292.5 0.5 522130NA18-03 294.8 295.8 1 522196NA18-03 295.8 296.2 0.4 522197NA18-03 315.2 316.2 1 522131NA18-03 316.2 317.2 1 522132NA18-03 318.6 319.6 1 522133NA18-03 319.6 321 1.4 522134NA18-03 321 322 1 522135NA18-03 322 323 1 522136NA18-03 323 324 1 522137NA18-03 324 325 1 522138NA18-03 325 326 1 522139NA18-03 326 327 1 522140NA18-03 327 328 1 522066NA18-03 328 329 1 522067NA18-03 329 330 1 522072NA18-03 330 331 1 522073NA18-03 331 332 1 522074NA18-03 332 333 1 522075NA18-03 333 334 1 522068NA18-03 334 335 1 522069NA18-03 335 335.5 0.5 522070NA18-03 335.5 337 1.5 522071NA18-03 344.8 345.8 1 522195NA18-03 389.3 390 0.7 522194NA18-03 403.5 404 0.5 522141NA18-03 404 405 1 522142NA18-03 405 406 1 522143NA18-03 406 407 1 522144NA18-03 407 407.5 0.5 522145NA18-03 407.5 408 0.5 522146NA18-03 408 409 1 522147NA18-03 409 410 1 522148NA18-03 410 411 1 522149

Ce_ppm_0.05

Co_ppm_0.1

Cs_ppm_1

Ga_ppm_0.1

Hf_ppm_0.02

In_ppm_0.02

La_ppm_0.1

Lu_ppm_0.01

Mo_ppm_0.05

Nb_ppm_0.1

Pb_ppm_0.5

Rb_ppm_0.2

Sb_ppm_0.05

Sc_ppm_0.5

Se_ppm_2

Sn_ppm_0.3

Ta_ppm_0.05

Tb_ppm_0.05

Te_ppm_0.05

Th_ppm_0.2

Tl_ppm_0.02

U_ppm_0.05

W_ppm_0.1

Y_ppm_0.1

Yb_ppm_0.1

56.28 17.8 9 20.7 1.93 0.08 28 0.14 49.73 4.5 74.6 109 0.2 8.9 2 2.5 0.44 0.34 0.23 3 1.13 1.23 2.7 9.7 0.855.97 19.9 7 19.1 1.52 0.11 26.7 0.12 50.62 3.6 38.4 89.1 0.17 7 2 2.5 0.39 0.38 0.19 2.5 0.97 1.17 2.3 9.5 0.959.28 23 9 19.8 1.82 0.12 29.8 0.16 52.75 4 32.2 106 0.18 11.4 3 2.9 0.29 0.41 0.25 2.3 1.21 1.24 2.7 10.8 156.96 15.8 7 21.1 1.91 0.07 28.4 0.16 34.86 4.8 33.9 105 0.21 11.6 <2 1.9 0.46 0.36 0.22 2.4 1.15 0.9 2.5 11 1

41.03 60 7 19.5 2.53 0.18 15.8 0.17 13.93 6.7 110 103 0.48 15.7 6 2.2 0.61 0.37 1.9 2.6 1.19 0.85 8.3 9.3 142.88 62.5 9 19.5 2.36 0.19 18 0.16 10.62 6 97.8 102 0.34 15 6 2.3 0.52 0.41 1.74 2.5 1.21 0.83 4.9 9.8 1

55.66 27.8 13 21.3 2.75 0.17 24.3 0.26 16.7 1.5 49.5 123 0.41 23.9 <2 1.7 0.11 0.61 0.86 3.2 1.17 0.86 1.4 17.7 1.654.81 30.1 13 20.6 2.62 0.11 24.8 0.21 15.8 3 51.1 114 0.36 18.1 2 1.8 0.16 0.49 0.74 3.2 1.12 0.89 2 15.9 1.4

66.57 61.6 9 22 2.22 0.14 30.8 0.26 19.17 6.1 82.2 125 0.42 15.2 6 2.4 0.5 0.66 1.43 3.2 1.17 0.91 8.9 19.1 1.754.1 59.2 8 21.8 2.37 0.19 24.1 0.23 16.86 6.7 177 129 0.4 15.8 6 2.2 0.5 0.56 2.42 3.1 1.11 0.9 16.3 16.2 1.558.3 57.3 8 23.2 2.5 0.18 25.7 0.21 19.59 8.4 106 134 0.43 18.2 5 2.8 0.63 0.52 2.12 3.3 1.17 1.01 23 15.5 1.4

56.75 63.5 10 23.3 2.49 0.18 25.2 0.23 29.13 7 71.1 145 0.49 20.3 6 3 0.51 0.52 1.37 3.4 1.35 1.06 14.1 16.5 1.458.69 59.8 9 24.5 2.65 0.17 25.8 0.27 19.12 6 189 154 0.73 19.3 4 3 0.51 0.55 1.9 3.5 1.42 1.14 17.3 17.5 1.754.14 63.8 10 22.4 2.52 0.17 24.4 0.21 27.52 5.5 89.5 143 0.66 15.8 6 3.1 0.5 0.54 1.78 3.5 1.35 1.03 10.5 17.7 1.458.76 65.8 11 26.4 2.92 0.18 25.9 0.29 29.25 9 32.8 157 0.62 21.3 5 3.4 0.71 0.61 1.48 3.8 1.43 1 7.6 21 1.961.43 42.6 8 22 3.32 0.12 28.7 0.27 35.76 9.6 54 122 0.37 15.3 3 3.6 0.73 0.57 0.84 3.6 1.13 1.09 9.7 16.9 1.776.8 38.7 6 17.9 3.15 0.1 37.5 0.24 124 7.9 278 97 0.42 7.6 6 5 0.62 0.63 1.36 3.3 0.88 0.99 7.2 17.3 1.6

77.77 8.5 4 17.6 4.89 0.08 34.5 0.25 21.84 15 40.2 92.4 0.23 4.1 <2 2.4 1.1 0.47 0.26 3.4 0.92 0.94 4.5 9.4 1.369.36 20.6 7 21.9 2.72 0.09 33.3 0.21 5.75 2.6 15.8 116 0.47 18.2 <2 1.8 0.19 0.53 1.05 3.5 0.81 0.92 8.3 15.3 1.4

41.36 4.6 2 18.1 3.98 0.08 17.2 0.28 4.05 12.4 31.5 59.4 0.2 4.3 <2 1.4 0.95 0.47 0.21 2.2 0.52 0.61 2.2 10.5 1.770.63 16.7 6 24.1 3.01 0.36 31.5 0.12 2.63 3.1 14.6 106 0.25 6.2 <2 1.6 0.34 0.47 1.46 4.1 1 0.95 7.4 9.8 0.762.11 9.1 5 23.2 2.24 0.25 28.2 0.08 1.71 2.7 70.3 99.8 0.29 4.6 <2 1.1 0.35 0.33 2.33 3.5 0.91 0.8 4.7 7.2 0.5

Page 4 of 4

MAPS

1ea,2c

2c,1ae

1b

1be

2cf

2c,1b

1cb,4ca

3b,10a1cb

3b

3b,S,(4a?)

1eb

OB1e2c1e

2c

2f

OB

1e

3b,2f,(1a)

1e

3f

1e,3f

1a,(3b)

3b,(1a)

1e

3b

1a,3b

1a,4a

1e,2f

3b

1a,4d

1bae,2f

2f,1a1a

2f

1ab

2bc1ab

2abc

3b

2f

10a,(2f)

2a

2c

1a,3a

1a

1a

3b

1a,4c

2a,1a

2f

2cf,1b

1ba,2fc

2f,1b

3b,2f

1b,2fc

2f

1b,2f

1a,2b

2f

2a,1a1b,2f

3b,4ba,1b2f

1bc,2f4

2f

1be

2f,1b

2c

1b,2c

3b,1a

3b

4b

4a

4b

1b

4d,gf

1a,gf

1a

1a

4b

6c

1a

6b

6b1b

1b

OB

4b

4bc,6a,gf

5a,1e

4cb,6a

4ba

2c1b,2fc

2fc1b4a

1b,2fc

4a3b

1b,10a

1c,10a

2cf,3b

1c

10a

4bdc

4bca

4bc,2

4a

4a4,2cf

4,2cf

6c

3b,4c

3b

2cf,3,6a

2f1b,2cf

4cb

4cb2f,4b

2fc

1e,2c

4cb

3b

4a

6a

4a

6a

1e

4bc

1b,3b

3b

3b,(2f)

2f,(3b)

1b,3b

3b

4b4a6a

4b

3b,(1a)

4b

1ba

1b,(3b)

4a

4b,1a

4ba

4a

4b

3b,1a

4b

1a

3b

6a

4a

4c,3b

6ab4cbe

3a3b

6a

3b,10

2f

4b,1

OB

4b

4e

2f,4e4e

2f,3b

2cf,3b

2f

2fc

10a2f,3b

2cf,3b

10a

2f,4

2fb4e

6b

4e2c

2c,3b

6ab

1b,4b

2b

2c

1b

2cf

1c

6a

2fc

1e1c

1a

4b,1a

6b,1a

6b

6b

4b,2f

6b5a

1a,4c

6b

1a

1a

1a

3b,(1a)4a

6a

3b

1a

1a

3b

4ba

4ab

4ab

4b,2f

4de

4a

6a

4ab

1e3b6a

1a,3b

1a6a

4a6a

1b3b

1a

3b6a2f

4a

3b,1a

1a,(3b)

4ab

1b

1b,3b3b

4abc

6c,(4b)

4e

4b

4b

1b1a

1a

2f,(1a,3b)

3b,(1a)

3b

1a,(3b)

3b

1b,2cb

2fb,1a

3b,6a

6a

3b

2cf

3b,6a,4e

6a,5b

3b,4e,6a

1a,2b

3b,6a

3b,6a4abe

1a,(3a)6a3b

3b

6a

6a,(3b)

6a,(3b)1a,(3b)

3b,(1a)

1a,(3b)

1b

2cb

3b,4e

6a

3b

6a

3b,4a

4dc6a

2f,4dc

6a

4dc

2f

1c

2f

2cf

3b

1bec

1b

3bf

2FC

4f

6a

3b

6a

2f

6a

2fb

3b,(1a)

2f,(1a,3b)

6a

3b

6a,(3b)

3b,1a3b

1a,(3b)3b

6a

2f,(1a,3b)

3b

3b

1a,3b

2f

1a

3b

1b

3b

1b

3b

1b,2c

3b4d,3b

2c,4a

2fc

1b,2acf

2c,1a

3b,1a

3b

3b,1a

6a

1a6a

1a,4b

3b

2f,(3b)

3b1a

1c

2f,1a

1a6b1a3b

6a

6c

3b

6c

2f

1be,43b,4b

3b

1be,2f

1b

2bf

2f

1aeb

OB

4b

6a

3b,2f

1a

3b,1a

1a

6a

4c,S,gf2a

4c

4cb

1b

1b1b

3b

1a,(2f)2f

3b1a,(3b)

1a,(2f)

3a

1a,2f3b,1a

6a,(3a)3a

1b1b1b,po

6c

3b

6c

1a

OB4b44c4e4c

OB4b,1b

10a,S

1c,4c

1c

1c,4c

10a,S,6a,4bc4bc

1cb,4

1b

1dc4c4c,1

4b

4bc

4b

4e

4b

4c,1c

2f

4c,1,24ce

1c,2

4bc1cb4c1c4c1c

1b1c,4

3b,4,4e3b,4

3b3b,4

1eb,2fb

6a

2fb,gf

3b

1be

1b

1d

BUR-01

BUR-03

BUR-04

B98-06

B98-08

Na-08-0

4

BUR-33

Na-08-0

7

BUR-44

B98-05

BUR-10

261-8

8-8

B98-01

BUR-55

261-8

8-9

BUR-58

Na-08-0

6

165-E

-1

BUR-46

BUR-11

BUR-47

165-E

-2

MK-9

2-9

261-8

8-13

HN-88-3

6

261-8

8-07

B98-07

Na-08-0

5

BUR-13

BUR-09

BUR-41

261-8

8-12

HN-88-3

5

BUR-35

BUR-40

BUR-34

261-8

7-6

261-8

7-2

261-8

7-1

BUR-53

BUR-38

B98-04

NA-07-

04

BUR-39

CC-1

BUR-24

MK-9

2-7

261-8

8-10

261-8

7-8

261-8

8-1

261-8

8-3

261-8

8-5

MK-9

2-8

NA-07-

07

BUR-57

BUR-37BUR-56

BUR-30

NA-07-

05

B98-03

BUR-49

BUR-18

BUR-50

BUR-17

BUR-48

BUR-29

BUR-19

BUR-26

BUR-27

BUR-28BUR-5

1

NA-07-

08

BUR-36

B98-02

NA-07-

01

BUR-20

BUR-23

NA-07-

03

261-8

7-3

NA-07-0

2

NA18-02

261-8

6-1

261-8

7-7

NA18-01

BUR-43

BUR-45

BUR-52

NA18-03

261-8

7-5

261-8

8-02

261-8

8-4

BUR-12

BUR-22

BUR-25

BUR-54

BUR-21

BUR-14

Na-08-0

3

Na-08-0

1

Na-08-0

2

HN-88-3

4

261-8

7-4

BUR-15

BUR-16

BUR-42

H-76-

1

261-8

8-6

HA-92-

06

HA-92-

02

HA-92-

03

HA-92-

04

HA-92-

05

HA-92-

01

POC-01

POC-02

HN-88-1

7

261-8

8-11

250

metres

500

North Abitibi ProjectDiamond Drilling Geology

Plan Map

Date: 12/20/2018

Author: M Ruhl

Office:

Drawing:

Scale: 1:10000


125

Projection: UTM Zone 17 (NAD 83)

0

Documents

accessible customer service. contact us. l’accessibilité ... · Tri Origin’s North Abitibi property is located in Hoblitzell Township, Larder Lake Mining Division, approximately