PETRO STUDY SUDBURY BRECCIA BELT 2 GARSON …...Geological Survey, Special Volume 4, Part l, pp. 593-625. Dressler, B.O. 1984: Chapter 4, General Geology of the Sudbury Area; in The

41I10SW2009 2.23781 GARSON 010 2 .2378 l

Petrological Study

on part of the

Sudbury Breccia Belt #2 Claim Group N.T.S.41I/11 SW

For

Wallbridge Mining Company Limited

Patrick Toth, B.Se. June 18, 2002

Table of Contents

Introduction..........................................................................................................................................................!

Location and Access ............................................................................................................................................J

Property History...................................................................................................................................................4

Topography.........................................................................................................................

Regional Geology.................................................................................................................................................^

Property Geology..................................................................................................................................................6

Exploration Surveys .............................................................................................................................................6

Conclusions and Recommendations....................................................................................................................6

Bibliography .........................................................................................................................................................7

Statement of Qualifications .................................................................................................................................8

List of Figures

Figure l: General Location Map Page 2 Figure 2: Property Location Map Page 3

Map Pocket

Geology and Sample Location Map

List of Tables

Table l: Claim Status Page l Table 2: Lithological Units Page 5

List of Appendices

Appendix A: Petrological Results

Appendix B: Assay Results

Introduction

On June 4th and 5 th of 2002, geological traverses were conducted across the Eastern block of the Sudbury Breccia Belt #2 claim group. The purpose was to locate and sample any Sudbury Breccia encountered for petrographic description and to verify the validity of previous mapping. Four rock types; arkose, greywacke, gabbro and false volcanics were encountered. 15 samples were collected for assay and petrological purposes.

Location and Access

The property is located in the northeastern corner of the Town of Sudbury, Ontario and is encompasses part of the Timberwolf Golf and Country Club. The claim block comprises Lot l, Con l, of Garson Township (figures l Si 2). The property can be most easily accessed by traveling east towards Garson along Hwy 86 and turning north onto Donnelly Drive. Follow Donnelly Drive north to O'Neil Drive West and turn left. Travel west for another 2 kilometers and cross over a set of railroad tracks. At this point, a foot trail heads southwest to the power line and the golf course. Walking west along the power line for approximately 100 metres bring one to the eastern claim boundary.

Claim Status

Property Name:Principal Commodity of Interest:Location:Township:Mining District:Province:Date of Acquisition:Renewal Dates:Operators Names:Title Status:

Sudbury Breccia Belt #2 GroupNi, Cu, and PGE'sLot 1J Con lGarsonSudburyOntarioJune22, 1999June 22, 2002Wallbridge Mining CompanyThe claims are wholly owned and are in good standing.

Table l: Claim Status

Claim #1222978

Size (units)7

Recording DateJune 22, 1999

Due DateJune 22, 2002

Figure 1: General Location Map

SRBB#2 CLAIM

Ontario

Figure 2: Property Location Map

LOT1

Lot 12

Con l

1222978

11

Property History

No past prospecting or mining activity has been recorded on the claim.

Topography

The property is generally flat with the exception of a large east-west outcrop ridge located along the northern portions of the claim block. Outcrop exposure consists of several small to medium-sized outcrops and outcrop ridges of low relief. The outcrop areas are largely devoid of overburden and any substantial vegetation. Overburden depth is generally very shallow. The southern portion of the claim block is low and comprises the Timberwolf Golf and Country Club.

Regional Geology

The Sudbury Igneous Complex is interpreted to have originally been a 200km diameter melt crater. The present expression of the now deformed crater is an elliptical form 65km long by 35km wide. It hosts some of the largest nickel-copper-PGE ore bodies found in the world. The geological history of the Complex has blessed it with numerous geologically diverse settings for the emplacement of nickel-copper-PGE deposits.

There are numerous volumes written about the Sudbury Structure and a more complete description of the geology can be found in the OGS Special Volume l, The Geology and Ore Deposits of the Sudbury Structure, 1984, edited by E. G. Pye, A. J. Naldrett and P.E. Giblin.

The 1850 Ma Sudbury Structure is located just northwest of the Grenville Geological Province, at the present boundary of the Superior Geological Province and the Southern Geological Province. The melt rocks associated with the structure consist of several basal units, some of which are critical to the deposition of sulphide ore bodies.

The "Main Mass" rocks consist of norite, quartz gabbro and granophyre while fine- to medium-grained quartz diorite and mafic norite breccias form the "Sublayer" at its base. The sublayer is host to much of the Ni-Cu sulphide ores of the Sudbury Structure which are emplaced in embayments at the contact with the crater walls. Granite breccias occurring at the base of the embayments also host the sulphides. Discrete radial and concentric offset dikes host nickel-copper-PGE deposits in a matrix of quartz diorite and associated breccias.

The impact at Sudbury formed pseudotachylytes (Sudbury Breccia) veins, melt bodies and Footwall Breccias that also contain appreciable economic mineralization. Differentiated sulphides rich in copper and PGE's are often found trapped in brecciated footwall rocks hosting Sudbury Breccia units and related melt bodies.

The basal units are overlain by various heterolithic breccias of the Onaping Formation and fluvial sediments of the Onwatin and Chelmsford Formations.

The Sudbury Structure has been deformed into its present day elliptical shape by northwesterly directed thrusting followed by regional metamorphism during the Leonean Orogeny. The 37Ma Wanapitei Lake Crater east of the Sudbury Structure also deformed the basin to its present shape.

Table 2 provides an overview of the numerous lithological units encountered in the Sudbury Igneous Complex.

Table 2: Table of LithologicalUnits

PHANEROZOICCENOZOIC

QUATERNARYRECENT

Organic deposits (peat bog); floodplain (alluvial) deposits

PLEISTOCENEGlacial deposits, glaciofluvial deposits, glaciolacustrine deposits

UNCONFORMITY

PROTEROZOIC

ARCHEAN

Olivine DiabaseINTRUSIVE CONTACT

Trap DikesINTRUSIVE CONTACT

Sudbury Igneous ComplexSublayerINTRUSIVE CONTACT Main Mass Gabbro

Whitewater GroupChelmsford Formation Onwatin Formation Onaping Formation

Black Member Grey Member Basal Member

Sudbury Breccia Footwall Breccia Shock Metamorphism

SUDBURYEVENT Nipissing Intrusive Rocks

INTRUSIVE CONTACT Creighton and Murray Granites

INTRUSIVE CONTACT Huronian Supergroup

Copper Cliff Formation UNCONFORMITY

DiabaseINTRUSIVE CONTACT

Mafic Plutonic Rocks and Anorthosite Intrusive; Contact Migmatite and Felsic Plutonic Rocks

INTRUSIVE (fe METAMORPHIC CONTACTMetavolcanic and Metasedimentary Rocks; Granodioritic-Quartzdioritic Gneisses and Associated Mafic Rocks

Property Geology

The Sudbury Breccia Belt #2 Property parallels the Sudbury Igneous Complex (SIC) over a strike length of 400m and is situated approximately 2.5km south of the SIC contact. The property overlays the South Range footwall rocks of the SIC. These are represented by the felsic meta-volcanics of the Copper Cliff Formation ^2460 Ma.). This formation is a member of the Huronian Supergroup (2100 to 2500 Ma.) and of the Elliot Lake Group respectively.

The property for the most part, is underlain by feldspathic wackes, quartz arenites and mafic flows of the Stobie Formation. Minor outcroppings of felsic tuffs of the Copper Cliff Formation can be observed in the middle of the claim block. Sudbury Breccia is also present in large quantities and can be most readily observed cutting the metasedimentary units. Metamorphism in the area ranges from lower-greenschist to amphibolite facies.

The metasediments weather brown weathered surface and a dark-gray in fresh surface. Grain size varies from fine to medium. Local cross bedding and grading are present as are minor polymictic and oligomictic pebble conglomerate beds. The metasediments have a granoblastic texture and contain porphyroblasts of hornblende, garnet and staurolite. Gabbro intrudes the metasedimentary and felsic volcanic rocks. The gabbro is generally dark green, medium to coarse-grained and is comprised of euhedral to subhedral amphiboles in a granoblastic matrix of feldspar, quartz and amphibole, chlorite and epidote. Hornblende occurs as radiating porphyroblasts and subhedral poikiloblasts. Trace amounts of pyrite and pyrrhotite are present.

Exploration Surveys

On June 4th and 5th , the eastern block of the Sudbury Breccia Belt #2 claim group was traversed and sampled. The work consisted of observing the outcrops traversed and taking grab samples of any Sudbury Breccia encountered for petrological and assay analysis.

Fifteen samples for petrological and assay purposes were taken at various outcrops on the claim block (map pocket). Samples PT-02-006 and 007 were described as narrow bands of Sudbury Breccia cutting greywacke. Sample PT-02-008 was described as a strongly foliated Sudbury Breccia in a well-bedded greywacke. PT-02- 009 was described as medium to coarse-grained, gabbro with radiating hornblende crystals. Sample PT-02-010 and 011 were described as strongly foliated Sudbury Breccias in greywacke. Sample PT-02-012 was described as a fine-grained, greywacke or quartz arenite. Sample PT-02-013 was described as a possible Sudbury Breccia in greywacke. Sample PT-02-014 was described as a medium-grained gabbro/amphibolite. Sample PT-02-015 was described as Sudbury Breccia in greywacke. Sample PT-02-016 was described as a medium to coarse- grained gabbro/amphibolite. Sample PT-02-017 was described as fine to medium-grained gabbro/amphibolite with possible Sudbury Breccia. Sample PT-02-018 was described as a strongly foliated, fine-grained gabbro. Sample PT-02-019 was described as a foliated and schistose greywacke with possible Sudbury Breccia. Sample PT-02-020 was described as a fine to medium-grained gabbro. The samples were cut, examined and areas to be thin sectioned were selected with the remaining portions being sent for assay. A detailed description of the petrographic work and the assay results can be found in Appendices A and B respectively.

Conclusions and Recommendations

Of the fifteen samples taken; 7 were Sudbury Breccia, 7 were gabbro/amphibolite and l was an arkosic metasediment. No significant assay values were returned. The Sudbury Breccias upon microscopic examination were found to be relatively "warm" in nature with textures ranging from fine-grained porphyritic to recrystallized. Given the large quantity of Sudbury Breccia on the property in conjunction with its close proximity to the known limit of the Sudbury Breccia Belt and several producing and past producing mines, a Total Field Magnetic survey might be warranted.

Bibliography

Card, K. D., Gupta V. K., McGrath, P. H., and Grant, F. S. 1984: The Sudbury Structure: it's regionalgeological and geophysical setting. In: The Geology and Ore Deposits of the Sudbury Structure. Ontario Geological Survey special volume l.

Dressler, B.O., Gupta, V.K. and Muir, T.L. 1991: The Sudbury Structure; in Geology of Ontario, Ontario Geological Survey, Special Volume 4, Part l, pp. 593-625.

Dressler, B.O. 1984: Chapter 4, General Geology of the Sudbury Area; in The Geology and Ore Deposits of the Sudbury Structure, Ontario Geological, Special Volume l, pp.57-82.

Innes, D.G. 1978: McKim Township, District of Sudbury; Ontario Geological Survey Prelim. Map P. 1978, Geol. Sen, scale 1:15840 or l inch to '/4 mile. Geology 1975, 1976.

John, G.W. 1996: Precambrian geology of Garson and Blezard townships; Ontario Geological Survey, Open File Report 5950, 47p.

Statement of Qualifications

I Patrick E. Toth, of the City of Toronto, in the Province of Ontario, Canada, do hereby certify that:

1. I am an exploration geologist residing at 42 Nursewood Road, Toronto, Ontario, M4E 3R8

2. I hold a B.Se., Geological Sciences degree conferred by Brock University of St. Catharines, Ontario in 1995.

3. I have practiced as an exploration geologist since 1995.

4. I am a member of the Geological Association of Canada, Canadian Prospectors and Developers Association of Canada, and The Canadian Institute of Mining and Metallurgy and Petroleum.

5. This report is based on personal examination and the implementation of work on the property on the dates of June 4th and 5th, 2002 on behalf on Wallbridge Mining Company.

6. I have no direct interest in the properties or securities of Wallbridge Mining Company.

Dated at Sudbury, Ontario,

this 18th Day of June, 2002 Patrick E. Toth, B.Sc.

Appendix A

Petrographic Descriptions

Sample # PT-02-006 Thin Section # W-02-0180

Hand Specimen Description: Narrow band of warm Sudbury Breccia cutting greywacke. Local gabbro raftswithin the greywacke.

Thin Section Description: Sudbury Breccia with abundant plagioclase spicules. Matrix is of intermediatecomposition with gabbroic/dioritic and sedimentary fragments and a fine grained, porphyritic texture.


Hand Specimen Description: Narrow band of warm Sudbury Breccia cutting greywacke. Local gabbro raftswithin the greywacke.

Thin Section Description: Sudbury Breccia with lineated plagioclase crystals. Matrix is of intermediatecomposition with sedimentary fragments and a fine-grained, porphyritic texture.

Sample # PT-02-008 Thin Section* W-02-0182

Hand Specimen Description: A strongly foliated Sudbury Breccia in a well bedded greywacke.

Thin Section Description: A strongly foliated Sudbury Breccia. Matrix is of intermediate compositionwith sedimentary fragments and a recrystallized texture.


Hand Specimen Description: A medium to coarse-grained gabbro with radiating hornblende crystals.

Thin Section Description: Coarse-grained, quartz-amphibolite. Quartz and feldspars crystals are in a fine grained mosaic with relict, sub-ophitic texture.


Hand Specimen Description: A strongly foliated Sudbury Breccia in a greywacke raft within gabbro.

Thin Section Description: A strongly foliated Sudbury Breccia. Matrix is of intermediate compositionwith sedimentary fragments and a fine-grained, porphyritic to recrystallized texture.


Hand Specimen Description: A strongly foliated Sudbury Breccia in a greywacke raft within gabbro.

Thin Section Description: A moderately lineated Sudbury Breccia. Matrix is of intermediate compositionwith sedimentary and gabbroic fragments and a fine-grained, porphyritic to recrystallized texture.


Hand Specimen Description: A fine-grained greywacke or quartz-arenite.

Thin Section Description: Fine-grained, biotite-quartz amphibolite.


Hand Specimen Description: Possible Sudbury Breccia in greywacke.

Thin Section Description: Fine to medium-grained, arkosic metasediment.


Hand Specimen Description: Medium-grained gabbro/amphibolite in contact with greywacke containingminor amounts of Sudbury Breccia.

Thin Section Description: Hornfelzed, oxide-rich, biotite-amphibolite.


Hand Specimen Description: Sudbury Breccia in greywacke.

Thin Section Description: Sudbury Breccia with a matrix of intermediate composition, sedimentaryfragments and a fine-grained, porphyritic texture.


Hand Specimen Description: A medium-grained, gabbro/amphibolite.

Thin Section Description: A weakly sheared, coarse-grained, quartz-hornblendite.


Hand Specimen Description: A fine to medium-grained gabbro with possible Sudbury Breccia.

Thin Section Description: A biotite-quartz-amphibolite with porphyritic hornblende crystals.


Hand Specimen Description: A strongly foliated, fine-grained gabbro with possible Sudbury Breccia.

Thin Section Description: Sudbury Breccia. Matrix is of intermediate composition with sedimentary andgabbroic fragments and a recrystallized texture in contact with a recrystallized, sub-ophitic quartz-amphibolite.


Hand Specimen Description: A foliated, schistose greywacke with possible Sudbury Breccia.

Thin Section Description: A recrystallized, medium-grained, biotite-amphibolite.


Hand Specimen Description: A fine to medium-grained gabbro.

Thin Section Description: A fine to medium-grained, recrystallized amphibolite-rich biotite-amphibolite.

Appendix B

Assay Results

XRAL XRAL LaboratoriesA Division of SGS Canada Inc.

Work Order: 068244 Date: 19/06/02 PRELIMINARY Page l of 3

lCO

ro CD CD ro

Element. Method. Det.Lun. Units.

W ALI 601 WAL1602 WAL1603 WALI604 WAL1605

WAL1606 WAL1607 WAL1608 WALL609 WAL1610

WAL1611 WAL1612 WAL1613 WAL1614 WAL1615

BLANK PC 102

AuFA3010.001g/mt

0.0020.0030.0140.0110.004

0.0040.0020.0050.0030.001

0.0020.0030.0010.0020.003

-o.ooi~o!o72

AuClFA3010.001g/mt

0.003—~—~

_-~~—-

-.

—

O.OOI..—

_

—

PtFA3010.010g/mt

<0.010< 0.010•CO.010< 0.010•CO.OIO

<0.010< 0.010<0.010<0.010•CO.OIO

<0.0]0<0.010<0.010<0.010•^0.010

<0.0100.276

PtCIFA3010.010g/mt

^TO.OIO—~——

_————

--

..

<0.010——

-p-

~

PdFA3010.001g/mt

<0.00l< 0.001< 0.001

0.003< 0.001

< 0.001*:o!ooi0.0080.001

< 0.001

0.0020.0020.002

•CO.OOl0.004

'CO.OOl0.53

PdClFA3010.001g/mt

< 0.001—~,--

_————

..—

0.002,-—

--

—

enCD"O

oo en

4^

O)

en

en ro

Member of the SGS Group (Societe Generate de Surx'eillancs) CDroCD

XRAL XRAL LaboratoriesA Division of SG S Canada Inc.

Work Order: 068244 Date: 19/06/02 PRELIMINARY Psge 2 of l

Clement.klrthod.)et.Lim.Jnits.

WALI60]WAL1602WAL1603WAL1604WAL1605

WAL1606W ALI 607WAL1608WAL1609WAL1610

WAL1611WAL1612WAL1613WALI614WALI615

BLANKAA CONTROL

AgAA73

0.3g/nit

•c:o.3<0.3<0.30.34

*C0.3

<0.3<0.3<0.3<0.3"^0.3

*C0.3<0.3<0.3<0.3t:0.3

<0.319.31

AgCIAA73

0.3g/ml

<0.3————

..————

,.--

<0.3——

_—

CD

roCD CDro

m c?CD

on CD-o nx:?o00

eaCO

x:

enj^.4^.en

en ro

Member of (he SGS Group (Socfett Generate de Surveillance) CDCO


Work Order: 068244

ent. lod.

VAL1601 Pr-oz-co6 VAL1602 Pr.oz.oo-* VAL1603 pr.o?-oo8 VALI604 pr-02-ooe VAL1605 C7.02- oioJVAL1606 IT-07.011 tV'AL1607 PT- at- oia. IVAL1608 PT- oz-013 IVAL1609 rr- 02 . 0/ y WAL1610 PT. ox. 0/5-

WAL1611 pr-c VAL1612 PT- oi. oi? VAL1613 PT- 02 -o 16 WAL1614 -pr-oz-oil VAL1615 rr 02 020

BLANK PG102

Date: 19/06/02 PRELIMINARY Pag* l Of 3

AuFA 3010.001g/ml

0.0020.0030.0140.0110.004

0.0040.0020.0050.0030.001

0.0020.0030.0010.0020.003

^.0010.072

AuClFA3010.00 1g/mt

0.003————

~———

_—

0.001..—

_

—

PtFA3010.010g/ml

*;o.oio<O.OlO<0.010< 0.010<O.OlO

*:0.010<0.010<0.010<0.010<0.010

-CO.OJO<0.010<0.010<0.010<0.010

•CIO.OIO0.276

PtCIFA3010.010g/mt

•c:O.OIO~~——

..^————

.m

..< 0.010

——

..—

PdFA3010.001g/Qlt

<0.00l<0.001<0.00l

0.003•CO.OOI

< 0.001< 0.001

0.0080.001

•SO.OOI

0.0020.0020.002

^.0010.004

< 0.0010.53

PdClFA3010.00 Lg/mt

< 0.001————

,.

————

K.

-.0.002

..—

—-

—

l

CO

ro CD

sc?

en CD

C/3

g

4^.

03

tn.c*.enro

Member of the SGS Gtaup (Societe Generate de Su^iHance)ro


Work Order: 068244

Element. Method. Det.Lim. Units.

W ALI 601 WAL1602 WALI603 WAL1604 WAL1605

W ALI 606 W ALI 607 WAL1608 WAL1609 WAL1610

WAL1611 WAL1612 WAL1613 WAL1614 WAL1615

BLANKSU1A

Dale: 19/06/02 PRELIMINARY Page 3 of 3

CuICAY50

0.010%

0.0132<0.010<0.010*C0.010<0.0]0

<0.0100.0103

•c 0.0 10"CO.OIO<0.010

0.02060.01640.0259

•CO.OIO<O.OIO

-CO.OIO0.9314

CuClICAY50

0.017*

0.013—..—-

—^-.—-.-

r ^—*

0.0264—-

™

-

Xi1CAY50

0.010'h

0.0102•CO.OIO<0.010<0.010<0.010

<O.OIO0.0199

*;0.oio<0.010<O.OIO

<0.010•^0.010<0.0100.01010.0171

<0.0101.1887

NiClICAY50

0.019fc

*C0.01——~-

_———-

. _,-

<O.OL——

, _

-

CoICAY50

0.010%

<0.010<0.010< 0.0 LO*c:0.010<0.010

<0.010<0.010•CO.OIO<0.010<0.010

<0.010<0.010*:o.oio<0.010<0.010

<0.0100.0359

CoCtICAY50

0.01•ft

<o.o~̂—~—_——

. ~--—

<0.01—"

,.

~

CDro CDCDro

mC3

CD

en CD-o

x:70

DO CO

J*.

en-e* .e* en

en ro

Member of the SGS Group (SocKte Generate de Surveillance)

70

CD

ONTMUO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Transaction No: W0270.01055

Recording Date: 2002-JUN-20

Approval Date: 2002-SEP-19

Work Report Summary

Status: APPROVED

Work Done from : 2002-MAY-15

to: 2002-JUN-19

Client(s):

392385

Survey Type(s):

WALLBRIDGE MINING COMPANY LIMITED

ASSAY MICRO

Work Report Details:

Perform Claim* Perform Approve

S 1222978 S3,530 S3.530 53,530 S3,530

Applied Approve

SO

Assign ReserveApprove Reserve Approve Due Date

O SO SO 2003-JUN-22

S3, 530 S3.530 S3.530 S3.530 SO SO SO SO

External Credits:

Reserve:

SO

SO Reserve of Work Report#: W0270.01055

SO Total Remaining

Status of claim is based on information currently on record.

41I10SW2009 2.23781 GARSON 900

2002-Sep-19 16:12 Armstrongjd Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date:2002-SEP-19

Ministers du Developpement du Nord et des Mines Ontario

GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5

WALLBRIDGE MINING COMPANY LIMITED 129 FIELDING ROAD LIVELY, ONTARIO P3Y 1L7 CANADA

Tel: (888) 415-9845 Fax:(877)670-1555

Dear Sir or Madam

Submission Number: 2.23781 Transaction Number(s): W0270.01055

Subject: Approval of Assessment Work

We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.

At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.

If you have any question regarding this correspondence, please contact LUCILLE JEROME by email at [email protected] or by phone at (705) 670-5858.

Yours Sincerely,

Ron Gashinski

Senior Manager, Mining Lands Section

Gc: Resident Geologist

Mark Hall (Agent)

Assessment File Library

Wallbridge Mining Company Limited (Claim Holder)

Wallbridge Mining Company Limited (Assessment Office)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:17541

MINING LAND TENURE

MAP

o oCN

S: o ut

o o

^^:iKI^ ,

•^•-•"' - - '/iY'; : --:;:: - v^V;1 ;,, h r./.:;? " ' c:

ii; i'w*.;*!-)"; 1 i N-;'i ?;T'i*M-;-*;' I"'*''l l* "'P''?n lfJsKf.wf f - *i'M- w, i soli's*-ff

P:F'' p:' : ' :: :."i;.' 3^ J ' : *'''WM jwiV's j:}*

Date /Time of Issue Sap 6 2001

TOWNSHIP l AREA

GARSON

14:25h Eastern

PLAN

G-4051

ADMINISTRATIVE DISTRICTS ; DIVISIONSMining Division Sudbury

Land Titles'Reglstry Division SUDBURY

Ministry of Natural Resources Ditlrict SUDBURY

TOPOGRAPHIC LAND TENURE

'a - a - a ,.^~.

El li",,'"D"'"""..-

E QaL .. .. - . . J

LAND TENURE WITHDRAWALS

E.ffi* i * "*l*^iflw|liomDh'" i"'UL"1****™*ta™ Mink* *n wmnf IM*I tjjiti

IMPORTANT NOTICES

LAND TENURE WITHDRAWAL DESCRIPTIONS

: yi*iirt

. (UKJ Wwi -Bi 1 21*11 nUMWIHU CLAWS JtptMlHOKATra r H Ml t'Ahlkg H t**LGF

l C bf ri l *T*iW SUB, (PI SE*1 M fit UlNlM ACT, FJLF TriAO

j HI" Wan Ait 1 2001 UC.t4^tOVL1ISLAttLJ HKO L*HD OHPEP WMI : '

j 94W Wtfii Ui1J(*1 QP3!U5ajl*a

WLL 117 i* t* HlVlfl M* 12 1H9 St t.3* YirtL tlFiflB Mil W*Y l i.DU UA&

IMPORTANT NOTICESAr*H loitti IW** ipn^lj

dikltif w*nintrit di**apm*rt

Dltft*feii[J**hDrwi*itfidufl. Tta* C ainalWMHi Hid Rtrui try irf

General Information and Limitations

may M a DB obtained ihnugh in lacH l^l Uktlmy nEnrd*i*'On~kc l al fn

Fa* H*^ t'u ml

Mn DffiiKi- HJU) IJ PinlKikn-MiTMIiMi iQfMiaijjprit D au som

tt m4y tt Mille Dining cldnii mn nut h* IkiaiMcd.

41I10SW2009 2.23781 GARSON

Documents

PETRO STUDY SUDBURY BRECCIA BELT 2 GARSON …...Geological Survey, Special Volume 4, Part l, pp. 593-625. Dressler, B.O. 1984: Chapter 4, General Geology of the Sudbury Area; in The