Upload
others
View
3
Download
0
Embed Size (px)
Citation preview
53D16NE8ee4 63.4856 BORLAND LAKE 010
GEOPHYSICAL INVESTIGATIONS
AT BORLAND LAKE, FAVOURABLE LAKE AREA,
RED LAKE MINING DIVISION, ONTARIO.
for
MASSIVE ENERGY LIMITED
by
J. B. Boniwell
Exploration Geophysical Consultant May 21, 1986
BXGAblBUR INTERNATIONAL GONSUbTftNTS bTD.
L53D16NE0004 63.4856 BORLAND LAKE
- l -
LIST OF CONTENTS
Introduction
Details of Survey
Data Presentation
Discussion of Results - A,
B,
C,
D,
IP/ResistivityMagneticsV.L.F. (radio) Em.Airborne Geophysics
Mineral Considerations
Conclusions and Recommendations
DV/G. NO.
EIC-16??-16?8
-16?9A,B-1680A.B
-1681A.B
-1682A.B
LIST OF DRAWINGS
TITLE
Page l
24
58
121315
. 20
010C
Locality Plan Showing Grid Area
Elements of Structure, Airborne Data
Chargeability Contours, Gradient Array
Resistivity Contours, Gradient Array
Magnetic Contours
Plan of Interpretation
SCALE
1:253,440
1:10,000
1:1200
li 1200
1:1200
1:1200
EXGAblBUR INTERNATIONAL CONSULTANTS bTD.
L L f
L L L L L
L
INTRODUCTION
A drilled mineralization rich in silver has been found to underlie parts of Borland Lake, about 250 kms. north of the town of Red Lake in northwestern Ontario. The mineral system is patently shear-controlled, and locally involves a number of irregular lenses of variable widths and grades. Strong lateral off-sets are evident in at least two localities. These conditions have rendered the task of adequately sampling the system awkward, but what has proven most difficult is the establishment of new extensions and repetitions.
Thus as an aid to on-going investigations, a programme of geophysics has recently been completed in the environment incorporating both lake and landward sections of the most prospective ground. This surveying has resorted to a combination of detailed magnetics and gradient array induced polarization (IP) applied systematically to supply a sought-after perspective.
The results obtained from this work form the basis of this reporting. They are however evaluated in conjunction with pertinent airborne data and some prior ground V.L.F. surveying in the area.
BXGAblBUR INTERNATIONAb CONSULTANTS LTD.
l s?
.
- r*
*'"'
1 -'A
fS'
*v* i
x*' '.
"i* H!
*L
A
l fc
l
-es
, f-l-.S
-*-^
-^/^
*i
'
' v*
A
V'
T
L,^
~
~i ~
Z~
^~~
*~\\
W+
f T T
rM
i
--v
^ 5*
.j*
* v
l t?
Z
* t
V:
U--^.'J
^.
y
l rr
* l
^/P
r* a"'
f^^
fe /i
s ^
/S l
-
W
t tv
t t-f
—
' 0
^L ^
en
~r ~
^.— -1
- —
H^
-
v*
. 5X
jf*^
F
-J^
- ^
^ -
V^
'CD
rr
v
f ^
*
'
L
L
950
530 -
/*
L
L-5I0 -
STOUT LAKE
DEER LAKE
Scale l ^ 20 miles
930
FINGER LAKE
FAVOURABLE LAKE
930
SANDY LAKE
Scale l - 4 miles
1985Airborne Survey
Area
Geophysical Grid Area
REDLAKE
BUSH PILOT CORPORATION
Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO
LOCALITY PLAN showing grid area
Dwg. No. E.I.C.-I677
- 2 -
L L L
L L
i_
DETAILS OF SURVEY
The grid lines prepared for this fresh coverage were laid
out due N-S at intervals of 50' and 100', The controlling E-W
base-line passed through the heart of the mineral system as it is
presently known.
The desired magnetic survey was completed with a Gem
Systems GSM-8 proton precession magnetomer providing measures of
the total terrestrial field to a sensitivity of l nT.- A reading
accuracy of about 3 nT has been achieved through the
contemporaneous on-site use of a fixed self-recording base
station magnetometer, Canadian Mining Geophysics MR-10,
monitoring geomagnetic field change every l min. during the
currency of the field work.
The IP coverage was carried out by gradient array
requiring the grounding of current electrode pairs at distant
sites approximately 3000' to either side beyond the limits of the
grid in the traverse direction. This is the so-called normal
mode of operation for the array. Up to l? lines 100' apart, were
surveyed from one current dipole set-up, and a further 18 from a
second. A total of 3400' in the BL direction were so covered.
Time domain equipment was employed for this operation,
specifically a Phoenix Geophysics IT-1 transmitter providing a
rated 3.0 kw of power working in conjunction with a Huntec Mk IV
receiver which yielded up to 9 channels of decay time
information. The measuring dipole spacing was kept at 100'
throughout the traversing, observations generally taken every
EXGAblBUR INTERNATIONAL CONSULTANTS bTD.
L
- 3 -
100' on line but were closed up in the immediate vicinity of the
.•showing to 50' .
L L L L
L
BXGAblBUR INTERNATIONAL CONSULTANTS MTD.
L
LDATA PRESENTATION
LL L
L
L
The collected data after suitable computation and
correction have been posted in plan and contoured. The plan
scale throughout is 111200.
Three parameters have been presented, viz. total field magnetics, apparent chargeability and apparent resistivity. The contour intervals vary for each, from 10 nT up to 1000 nT for the
magnetics, 0.5 millisec for the chargeability and 100 to 1000 ohm-metres for the resistivity. Contouring has been undertaken
by hand for all three parameters.
Features brought out by the subsequent interpretation of these results have been compiled into a suitable overlay.
As part of the current evaluation, consideration has been
given to the airborne geophysical results which were recorded in an earlier surveying of the region. These data included
magnetics, V.L.F. (radio) em. and conventional frequency em. measurements collected by low level helicopter flying under the
guidance of (Mini-Ranger) electronic navigation. The chief interpreted elements of structure and lithology perceived
therein, which pertain to the present ground search area, have
been compiled at a scale of 1:10,000. This hews to the base scale of all the air-data presentations and thus allows
correlations therewith.
LBXGAblBUR INTERNATIONAL CONSULTANTS bTD.
L
- 5 -
DISCUSSION OF RESULTS
L A. IP/Resistivity (Dwg. Nos. EIC-16?9, 1680)
L
These results are accorded priority since they are likely
to reflect most directly the mineralization itself. A singular
showing (the Johnston showing) at the lake edge offers a valuable
control.
Thus it is promising that at the western shore of Borland
Lake where this best exposure exists, a recognizable
chargeability anomaly has been obtained in correlation. In
amplitude terms, it is quite a modest response, two and a half
times background at best, but it is unmistakable. It is
constrained in size, and is also accompanied by a heightened
resistivity locally which implies an attendant silicification.
All this fits well the manner and style of the mineralization as
it has been revealed and defined by drilling.
It is therefore remarkable, and of extreme pertinence to
exploration prospects in the area, that this anomaly does not
behave in a predictable fashion. While to the east there is a
discernible tail extending out into the lake broadly on strike,
there is nothing comparable to the west. Instead, the anomaly
there swings sharply to the south-west, and stays on this course
for nearly 300' before petering out. That this is no weird
aberration of data is confirmed by the resistivity results which
behave even more pronouncedly in the same manner. It appears
BXGAblBUR INTERNATIONAL CONSULTANTS bTD.
l
L L
- 6 -
probable therefore that the mineral zone has been warped in this
way under the influence of cross-structure,
Once this concept is accepted, several possibilities open
up. The responsible structure here is projected to be a NE fault
which lies just off-shore, and so has been hidden from past
conventional mapping. It also seems to have escaped drilling!
certainly it has not been tested in any section where the results
would be telling and umambiguous. Importantly, this cross-fault
intersects the known vein system where the best mineralization
appears to be concentrated j for example, the intercept obtained
in DDK #65-2 wherein an average 12.5 ozs. Ag over 109,4' (33-35
m) was recorded occurs in the vicinity, and it is the premier
intersection of the drilling so far. Since immediately adjacent
holes failed significantly to match this intersection, the
inference can be drawn that the main zone has indeed swung off
the drill grid, or has been locally interrupted.
Potentially then cross-structures form a critical part of
the mineral setting in this environment. This likelihood however
may not make exploration any easier. It implies instead that
rather than one coherent mineralized system, there will be a
number' of broken up bodies., possibly of different ages, and
occupying a variety of positions and attitudes.
This indeed appears the case. Further afield on the
grid, such polarization anomaly that has been obtained occurs in
a scatter. There is no strong sense of a governing throughgoing
system. Nonetheless several of these individual events are -in-
EXGAblBUR INTERNATIONAL CONSULTANTS bTIX
l
- 7 -
L
triguing in themselves. Manifestly the most notable, -- it being
one of the strongest polarization features of the survey has been encountered on lines 15W, 16W as they straddle the edge of
Solon Pond. The high positive centre is flanked by some equally
low troughs, and the indication is that current flow threading
this sector has been radically distorted by contravening current
paths. The effects are typically local and pronounced. It is
considered most probable that cross-faulting has wrought at least
part of this disorder, although the strike bearings of the axes
involved are not immediately evident. Resistivities tend to be
unhelpful in this regard as they drop environmentally to extreme
lows. In all, this is a very remarkable locality, and its
significance is more specifically addressed in a later sector.
Among other chargeability features of the area is a zone
of high which emerges from Borland Lake at 500S/2000N in the
southern quarter of the area. It is accompanied by lowered
resistivities and although in part due to the lake itself, this
is a characterizing condition that se'ts it apart from the
Johnston mineralization. It is also an incomplete anomaly,
remaining open to the east.
To the north-east of the showing sector, a complex Of IP anomaly has been obtained} in fact all across the northern
reaches of the grid, a sprawl of anomaly exists, much of it
untidy and locally irregular. Several sources are presumed
present, some of them ostensibly formationally controlled, others by structure. High resistivity correspondence appears in two
places, viz. at 650N/300E and at 1250E/1900W} and in both .
instances outcrop is present. It follows these rocks should be
BXGAblBUR INTERNATIONAL CONSULTANTS LTD.
L
- 8 -
L-
l
closely examined and sampled, both for their chargeability propensities and their mineral content, particularly in the first location where considerable shearing and carbonitization have been mapped in felsic volcanics.
In this general vicinity, the evidence that structure is also contributing to anomaly distribution is chiefly supplied by the lobe of chargeability response which extends SW towards the Johnston showing. It does not quite reach that far but its on-strike affinity with the arm which does extend south-west beyond there is unmistakable. Increasingly it appears that this particular axis forms part of the mineral history of the
environment, albeit in this latest section resistivities do not
climb typically, but drop off, presumably in part because of the effects of the lake. Moreover in this neighbourhood there appear again some strange peak IP highs and lows which, although much more confined, hark back to the Solon Pond situation. Since transgressing structure is strongly suspected in that first case, so ought it be here in the second.
Again therefore this is an interesting locality with more
than one facet to consider and sample.
B. Magnetics (Dwg. No. EIC-1681)
Dramatically, the main drilled mineralization provides an anomalous trace in the obtained magnetics.. This was not expected. The expressions involved amount to 400 nT in local
BXGAblBUR INTERNATIONAb CONSULTANTS LTD.
- 9 -
relief, and their correlation with the mineral system is faithful and undeniable. An ultramafic finger, presumably a sill, approximately 6' wide, appears in the drilling about 200' to the south side of this argentiferous zone, and is potentially a factor, but where fair comparisons can be made, it is not a major one. It seems that there is enough pyrrhotite extant in the mineral assemblage to account for most of the observed effects here.
ii_
Whether this association represents a general condition for the area however suddenly becomes a crucial question, for it is evident that the zone of magnetic anomaly does not extend in any strength beyond the limits of past drilling. Even more disconcerting, it does not follow the IP through its apparent curve to the south-west across lines 200W et al. At issue is whether the magnetics are more accurately reflecting the important mineral incidences of the area, or whether the IP results are.
If it is the magnetics, then it is clear not too much more can be anticipated from the on-strike possibilities of the main zone. Some weak anomaly across lines 700W-900W, and a couple of very confined, semi-isolated peaks positioned around the edges of Solon Pond virtually represent the entire potential for new occurrence to the west. Despite their strength, there is little encouragement inherent to either of the latter events. To the east, it is possible to suppose extra extension as the zone closely approaches the peridotite intrusion in the lake, on the assumption that all magnetic definition of it is lost to the overwhelming influence of the ultramafic. But this of course is
EXGAblBUR INTERNATIONAL CONSULTANTS LTD.
- 10 -
largely speculative, notwithstanding the hints in drilling of mineralization on the intrusive (south) flank. More to the point is the clear indication that magnetic anomaly does not conform to the principal IP/resistivity ridge which extends eastwards from the Johnston showing. This circumstance implies that the magnetics in following the known mineralization is tracing in effect the locus of the host shear; the IP/resistivity alignment (heading due east) must thus be describing a separate system, whether formationally or structurally controlled.
It therefore becomes important at this stage to look' at the other features the magnetics supply. There are two other zones of anomalous high. One in the northern parts of the grid, circa 900N, lines 500E-200E, denotes the presence of an iron formation according to outcrop evidence. This is neither a large system nor a strong one, but it implies a bedded unit relatively rich in magnetite. As such, it promises a useful marker for the environment. Unfortunately, it is neither very extensive here it quickly strikes off the grid -- nor is it distinctly a chargeability.
Across the south-west corner of the grid, a stronger, more compound magnetic system appears. It too follows a broad WNW orientation, and in consequence it might also be formational in origin, However in this instance, there are far more irregular components present. As a result, the system could indicate a string of several ultramafic pods, or more evocatively, a broken up sill of similar material potentially disposed about a synclinal fold. Small outcrops of peridotite appearing where the system crosses the shorelines of Borland Lake
EXGAblBUR INTERNATIONAb CONSULTANTS LTD.
- 11 -
l
and Solon Pond reinforce the source probability at least.
To the west of Solon Pond, a broad high of magnetics
supposes that another large ultramafic intrusion occurs there,
again in a locality of little or no outcrop. This feature
remains open to the west, and according to the aeromagnetics
extends for approximately another 1500'.
Given all these intimations of ultramafic intrusion in
the grid area, the weight of evidence suggests that, of the two,
the IP data are more indicative of sulphide mineralization in the
environment than the magnetics. This of course is not too
surprising a 'conclusion, but it can not be taken very far since
-- inevitably it seems -- there is always some polarization
associated with the ultramafics, and some of this response is
undoubtedly due to magnetite. Still the hope remains that there
exist interesting sulphides in the area which contain no
pyrrhotite or magnetites and it is these sulphides which loom as
the new targets for exploration if mineral potential is to be
materially increased here.
Beyond these considerations, the magnetics do not reveal
much in the way of background geology, due. largely to the lack of
contrast across the bedded lithologies. The further fresh
insights to be obtained are all structural in connotation, and
these are evaluated in conjunction with other data, especially
including the V.L.F. em.
BXGAblBUR INTERNATIONAL. GONSUbTftNTS bTD.
- 12 -
C. V.L.F. (radio) Em.
L
Some earlier acquired ground V.L.F. em. data (1985) can
be usefully integrated into present considerations. Although
coverage is more limited than both the magnetics and IP, and was
effected on a differing grid from one transmitter station only
(NAA, Cutler, Maine, broadcasting at 24.0 kHz), there are some
anomaly features which merit note.
The pre-eminent results in the current context is the
anomaly expression which has been obtained in direct correlation
with the showing mineralization. This correspondence, so far as
the coverage allows, starts and ends with the main zone as
defined by drilling. Thus V.L.F. surveying confirms what the
magnetics have already implied: further on-strike extensions of
the silver zone appear limited.
Yet there is evident considerable V.L.F. anomaly aligned
in sub-parallel systems. Several of these might be ascribed to
lithologic boundaries within the formational sequence, that is,
they are run-of-the-country events, but most are likely due to
shears'. For example, a good case can be made for the anomaly
axis which borders the north shore of Borland Lake since shears
in felsic volcanics have been mapped locally here. However what
remains most of interest to present considerations is the
indication of cross-structure in these data.
Unhelpfully, the lines of the V.L.F. grid run virtually
in the same direction as the critical, most strongly postulated
BXGftblBUR INTERNATIONA!, CONSULTANTS bTD.
L
L
L
- 13 -
cross-faulting, that is NE-SW. Resolutions in consequence are
very poor. Just the same, some clues to such faulting do reside
in the (contoured) results. In addition there is indication from
place to place of N and NW faults. Their significance is
unknown.
Taking all the signs of cross-structure together,
absorbing as well those furnished by the airborne geophysics, the
fault axes which appear most realistic to the area are as shown
(Dwg. No. EIC-1682). As can be seen, the NE-SW set appears to
dominates these faults find support in all methods. Only the
shears, or strike faults have a stronger combination of
expression, partly because they are more frequent, and partly
because they have been favoured by the grid (and flight path)
orientation.
D. Airborne Geophysics
In 1985, Aerodat Ltd. were contracted to overfly the
Borland Lake sector as part of a wider coverage. Besides
magnetics and V.L.F., measurements were collected with conventional em. (operating frequencies 9^6 Hz, 4575 Hz).
However no em, anomaly was recorded within the present grid area.
The magnetic and V.L.F. results on the other hand provide
evidence of anomaly trends which cross the area at a scale that
is regional in scope. Thus the mineral zone is largely not seen
for itself in either data set, although the magnetic ridge across
BXGAblBUR INTERNATIONAb CONSULTANTS LTD.
L
the Johnston showing point does make itself evident; nevertheless
in this presentation it appears confusingly as a westward poking
tongue merely of the ultramafic intrusion in the lake whose
anomaly commands this locale.
As to be expected, the skein of ultramafic bodies in the
south of the grid area appears as a more homogeneous whole in the
air-data, and as already noted, more extensive. While these
kinds of melding do not aid the present interpretation
particularly, overall they do supply some sort of perspective.
Thus the larger regional faults can be seen with more clarity at
this scale than at the grid scale, and it is in this regard, the
airborne data make fair contribution.
As foretold, the strongest cross-breaks occur on the
NE-SE orientations there appears a family of them in the region.
But really for the first time, structures with N-S headings
become manifest. One of them passes through Solon Pond, and as
will be implied, this could be important to future mineral
chances.
BXGAblBUR INTERNATIONAL CONSULTANTS bTD.
L.
L.
- 15 -
MINERAL CONSIDERATIONS
To begin with outcrop, the showing mineralization at the lake edge has provided geophysical responses in chargeability, resistivity, magnetics and V.L.F. em., all in fair coincidence. It would appear therefrom that projections of new occurrence ought to be straightforward. However in fact, they have proven far from simple.
This is because outside this one locality, there is no repetition of such a convergence of geophysical events anywhere else in the area, even along the immediate strike of the mineral zone as it has been outlined by drilling. It appears in consequence there are a number of divergent factors controlling mineralization in this sector, not all of which have previously been recognized.
Tackling the most logical possibilities first, viz. the on-strike extensions of the WNW fracture system passing through the showing setting, it is suggested by correlating resistivity and magnetic highs that this axis weakly reappears after an interceding break to pass through 250N/700W going on to 350N/900W. Over the relatively short 300' strike distance involved, there is exhibited a combination of modest magnetic and resistivity high, and it seems fair to add it to the strike extent of the showing system, especially since there is a weak companion IP anomaly at the east end. However there is no persistence, and V.L.F. tends to veer away southwards to pass it by. Moreover, a drill hole, #65-23, appears to have already
BXGAblBUR INTERNATIONAL GONSUbTANTS bTO.
- 16 -
probed this weak feature, presumably without notable success.
To the east of the showing out into Borland Lake, the V.L.F, and magnetic correlations are maintained on strike, but disconcertingly, both the mainstream resistivity and polarization anomalies quickly diverge from the known mineralization, and in consort hew to an independent (due east) course. On closer examination, it can be seen that a weak tail of IP and resistivity high does in fact stay with the drilled mineraliza tion in its ESE extension, but that in the circumstances it is having difficulty making itself discernible.
All this means that there is much more contributing to geophysical anomaly in the area than the known silver zone. It follows that there is an urgent need to understand and identify these other components since they patently impinge on any widened mineral possibilities inherent to the geology of the environment,
There are two immediate targets to concentrate on. One is the strongly developed arm of resistivity and polarization anomaly which strikes SW from out of the showing setting. There is some V.L.P. evidence to suppose that this is a cross-structural fault alignment, and the attendant IP/resistivity responses suggest in consequence that some of the silicic mineral fluids in the silver fracture system have at the time of their incursion taken advantage of this intersecting line of weakness. However there is no comparable magnetic high in correlation; if anything, this zone is distinguished by a slight lowering of magnetic level locally. This infers an absence of pyrrhotite and of ultramafic intrusion both; and that fact may
EXGAblBUR INTERNATIONAL. CONSULTANTS LTD.
- 17 -
well signify that there are two kinds of mineralization and two
ages of veining present and threading the area.
If so, this second generation of occurrence has not been drilled, or for that matter sampled in any diagnostic way. There is no perceived reason why it should not carry precious metals, and that possibility alone is warrant enough to undertake its
early testing.
From this widened point of view, it appears of some moment that much of the IP anomaly recorded in the areas has a NE-SW bias at the same time as it attempts to follow E to ESE formational trends. The second target of priority interest embodies this twin influence but with a twist: the polarization axis appears almost N-S while the resistivity trends of the locale are almost E-W. The anomaly in question centres upon 600N/1600W on the edge of Solon Pond. The polarization involved nearly reaches ?0 msec., or that is more than twice that of the showing anomalyj moreover it is accompanied, not by a resistivity high, but by a vast low which drops to an extraordinary level of 2? ohm-metres and less locally. Even the latter however is not confined to the chargeability but embraces an area roughly ?00' x 500' within a bay of Solon Pond. At the same time, there have been recorded within this realm some very large chargeability negatives adjacent to the positives. These infer, not inductive effects per se, but current reversals due to rather unusual body geometries and/or source dispositions. The very low resistivities themselves are believed primarily due to a clay which must come virtually to surface in places within.
BXGAblBUR INTERNATIONALCONSULTANTS bTD.
L
- 18 -
There is a lot to be explained here. The whole of this bay in one way or another is anomalous. Aside from the magnetics which are expressionless, the surrounding geophysics reiterates
the exceptional character of this locality. Nor is the behaviour of anomaly anything to do with the lake itself. That is evident just from the localization that has taken place within it. There
is too the sense of a centre, with bands of IP effects curving around it. The V.L.F. coverage unhappily is very skimpy right in
this section, but what results do exist demonstrate that strong
anomaly surely underlies this bay.
The most favoured interpretation of these remarkable
circumstances is a clay alteration product that has been
developed in a locality of great structural interaction. One
important aspect of this Solon Pond clay deposit is that it lies directly on strike with the (Johnston) silver zone fracture
system. Also it seems highly probable that a N, or NE bearing fault has intersected it here. The quasi-circular outline of the
bay, even, evokes images of a vent, that is, a brecccia pipe, raking NNE, perhaps in-filled by a (felsic) intrusive plug coming up it to near-surface. Whether this is a valid premise remains to be seen} also whether such a pipe would form a primary source to the silver mineralization likewise is unknown. But it is clear that there are discrete finite sources of polarization potentially due to metallics in this unique setting which beg to
be investigated.
What is learned here can then be transferred to two
lesser possibilities which unexpectedly exist to the ENE. In IP
terms there are similarities, the strong sharp highs for
EXGAL.IBUR INTERNATIONAL CONSULTANTS LTD.
L
- 19
instance, and the rapid drop in resistivities, even a small negative polarization in one place, but the scale differs and there is no one centre. As before, intersecting fault structures are present, also as before, the magnetics are indifferent, but this time there is much more polarization about, and a fissure-type mineral emplacement seems more appropriate in consequence. There is no question this sector is interesting, and it too deserves follow-up, but more for itself than a stretched analogy with the Solon Pond events.
BXGAblBUR INTERNATIONAL CONSULTANTS bTO.
- 20 -
CONCLUSIONS AND RECOMMENDATIONS
Some very intriguing results have been obtained by the combined geophysical surveying recently completed. They have also provided several surprises which will require eventual reconcilation with geplogy and the mineral probabilities of the area.
As things stand, the known silver mineralization has little conventional strike potential beyond the limits of drilling according to geophysics. A weak 300' extension across lines ?OOW and 900W is about all that can be forecast.
However, there are much wider possibilities for mineral occurrence in the area if several of the non-analogous, non-conforming anomaly features obtained in survey are ever found to represent emplacements of significant precious metal mineralization. Specifically there has emerged evidence severally of mineralized cross-structures, of bedded sulphidic horizons, and most unusually, of vents containing metallics. The most outstanding of the latter occurs in the pronounced north eastern bay of Solon Pond, most apparently affecting the shape . and style of this physiographic feature and surrounding terrain.
It is judged that at least three of these "outside" possibilities ought be subjected to intensive investigation, including drilling, in the next stage of exploration.
Increasingly i-t appears that the whole of the grid area constitutes an unusual mineralized environment, conspicuously
BXGALIBUR INTERNATIONAL CONSULTANTS LTD.
- 21 -
spearheaded by the argentite mineralization of the Johnston zone.
There is much to learn here, and it is believed there are new and exciting prospects in the area that have yet to be discovered.
It is therefore recommended that the following steps be
undertaken}
i) all available drill core from past drilling on the silver zone be logged systematically by magnetic
susceptibility meter, and appropriate down-hole
profiles plotted;
ii) all other evidence of sulphides in the same core be
noted and plotted on section and in planj
iii) these data be reconciled with present geophysics!
iv) the rock outcroppings in the vicnity of 650N/300E,
and around 1250N/1900W be examined and sampled
geochemically for precious metal indication. In the
latter locality, the so-called Solon No. l Zone
prospect needs to be fixed with respect to the
present.grid j
v) on the basis of findings, a programme of diamond
drilling be embarked upon, the holes testing within
the showing environment and along its structural
strike such possibilities supported by geophysics
and seemingly not previously sampled adequately.
This could include the evident system extension
BXGflblBUR INTERNATIONAL CONSULTANTS bTD.
vi)
vii)
viii)
ix)
- 22 -
across lines 700W-900W.
notwithstanding any of the foregoing, the Solon Pond breccia pipe concept be drill-tested on its own merits. A suitable hole for the purpose would be i
DDK #86-Glt Collar at 750N/1400W
to be drilled grid SW at -50 for 450'
as for vi) above, a hole be drilled into the noted IP/resistivity zone branching south-west from the main (Johnston) showing location. Again a suitable
hole would be i
DDK #86-G2: Collar at 100N/300W
to be drilled grid SE at -50 for 350'
the complex of apparently structurally controlled IP
anomaly to the grid north-east be drilled as part of
the widened search for new mineral occurrence in the
area. An appropriate hole would be i
DDK #86-031 Collar at 600N/00to be drilled grid S at -50 for 450'
consideration be given to extending a complete V.L.F,
coverage to the present grid area. It ought be
possible to obtain concurrently on these lines
measurements in both the broadcast fields of NLK
(24.8 kHz), Seattle, Washington, and NSS (21\4 kHz),
t BXGAblBUR INTERNATIONAL CONSULTANTS LTD.
- 23 -
Annapolis, Maryland, to the considerable benefit of the overall programme.
x) future IP surveying be planned if the proposed tests prove encouraging.
The above cited drilling totals 1250'. This footage provides a reasonable minimum to initiate a test programme in the area, especially since all targets in each case represent potentially a new mode of occurrence. The holes are all collared on land to permit summer drilling if desired.
Finally it is concluded that if these recommendations are adopted, then a much better idea of the overall mineral potential of the environment will ensue. Besides that, the very testing herein provided may well furnish direct evidence of other important mineralization beyond the known silver zone, This eventuality, if it comes to pass, would of course open up a spate of new possibility, not just for jUhe 'immediate search area, but for the region as a whole.
May 21', 1986. J. B. BoniwellExploration Geophysical Consultant
BXGAblBUR INTERNATIONAL CONSULTANTS bTI).
53D16NE80a4 S3.4856 BORLAND LAKE
REPORT ON THE
1986 DIAMOND DRILL PROGRAM
AT THE
BORLAND LAKE PROPERTY
FOR
MASSIVE ENERGY LIMITED
SEPTEMBER l, 1986 Toronto, Ontario
Kenneth W. Johnson Project Geologist
53D16NE80M 63.4856 BORLAND LAKE020C
LIST OF CONTENTS
Introduction Page l
Property Location and Description l
Description of the Diamond Drill Program 5
Geology of the Borland Lake Deposit 5
Results of the 1986 Diamond Drill Program 6
Conclusions and Recommendations 7
Recommended Program and Proposed Budget 7
Appendix: Diamond Drill Reports No.'s 86-1 to 86-6 10
LIST OF DRAWINGS
Figure l
Figure 2
Figure 3
Figure 4
Figure 5
Property Location Map
Property Map - Borland Lake Area
Grade Thickness ContoursBorland Lake Deposit
3
4
Map Pocket
Plan of Diamond Drilling Map Pocket (l inch = 100 feet; E S. W sheets)
Longitudinal Sections showing Tonnage Map Pocket Blocks (i inch = 40 feet)
-2-
STAKED CLAIMS
KRL 697239 - KRL 697291 inclusive KRL 775009 - KRL 775043 inclusive
PIC LAKE AREA
53 claims 35 claims
Total Staked Claims 88
TOTAL NUMBER OF CLAIMS 98
At the present time Title to the above 98 claims is held by Noranda Exploration Co. Ltd. Under the terms of a Joint-Venture Agreement with Noranda dated February l, 1986, Massive Energy Ltd has earned a 59.8476% interest in the property through the expenditure of $216,029.95 on exploration during the period February l, 1986 to August l, 1986 (Massive Energy Ltd, unaudited statement, August l, 1986).
The following claims staked in 1984 and 1985 are held outright by Massive Energy Ltd. They were staked in order to cover the favourable geological formations between the Borland Lake and the Pic Lake claim groups.
28 claims43 claims41 claims3 claims6 claims2 claims2 claims2 claims4 claims4 claims3 claims
26 claims8 claims
KRLKRLKRLKRLKRLKRLKRLKRLKRLKRLKRLKRLKRL
793882823497823547823590823595823607823615823623823649823657823665823671828199
- KRL- KRL- KRL- KRL- KRL
KRL- KRL- KRL- KRL- KRL- KRL- KRL- KRL
793909823539823587823592823600823608823616823624823652823660823667823696828206
inclusiveinclusiveinclusiveinclusiveinclusiveinclusiveinclusiveinclusiveinclusiveinclusiveinclusiveinclusiveinclusive
TOTAL STAKED CLAIMS 172 Claims
Massive's 1986 diamond drill program concentrated on the Borland Lake silver deposit which lies within claims KRL 49061 and 49065.
x x
l /GODS'LAKE
MANITOBA s-3-
HUDSON BAY
V ONTARIO
.LINGMAN LAKE
BORLAND LAKE
Red * Lake
kenora
MUSKEGSAGAGEN LAKE
Thunder Bay-
PANGIS
USA
Timmins/)
^Sault Ste. Marie
QUE BEC
CASA BERARDI Matagami
Val d 'Or
Ci'rklqnd l Lake
Toronto
MASSIVE ENERGY LTD
LOCATION MAP
BORLAND LAKE PROPERTY
INTRODUCTION
In May 1986, Massive Energy Limited completed a limited diamond drill program on the Noranda-Optioned Borland Lake property in Northwestern Ontario. The program consisted of six diamond drill holes, totalling 3032 feet, designed to test the silver-bearing zones at and below the 300 foot level, and test an area closer to the surface where mineralization had not been established. Drilling by Noranda Explorations prior to 1969 established Probable Ore Reserves of 244,493 tons at 8,27 ounces per ton silver and 0.02 ounces per ton gold. Noranda's exploration delineated the mineral ization to the 250 foot level over a strike length of 1200 feet.As a result of Massive's drill program, the Probable Ore Reserves now stand at 431,967 tons of 8.43 ounces per ton silver and 0.02 ounces per ton gold.
An exploration program consisting of approximately 8000 feet of diamond drilling is recommended to substantially increase the drill indicated tonnage at Borland Lake, and possibly locate other silver-gold deposits either parallel to or along strike of the main deposit. The total cost of the proposed program, if fully implemented, is estimated at $350,000.
PROPERTY LOCATION AND DESCRIPTION
Massive's Borland Lake property is located 125 miles north of the Red Lake gold camp and 50 miles east of the Manitoba border. The property is comprised of a block of 10 leased claims and a contiguous block of 260 unpatented claims for a total of 270 mining claims covering approximately 10,800 acres. Specifically the claims are as follows:
LEASED CLAIMS
Lease No.
102651
102652
BORLAND LAKE AREA
Claim No s.
KRL 49063 KRL 49065 KRL 49066 KRL 50256 KRL 50257
KRL 49059 KRL 49060 KRL 49061 KRL 49062 KRL 49064
Total Leased Claims 10
-5-.
DESCRIPTION OF THE DIAMOND DRILL PROGRAM
A total of 3032 feet of BQ core was drilled in six holes during the period from March 15 to March 29, 1986. The drilling was supervised by the author, and was contracted to M Si B Drilling Ltd. of Powell River, British Columbia, who utilized a Boyles B.B.S. - 15 diamond drill which has a depth capacity of approximately 1000 feet.
The drill equipment was mobilized into Borland Lake via D.C. - 3 and Otter aircraft, and was transported to each drill site by a Bombadier J-5 muskeg tractor. Each drill hole was located and spotted with respect to a chained and picketed grid, with the baseline oriented at 097".
All drill holes were inclined to the north at 45 to 60 0 angle, and were cased through approximately 100 feet of clay overburden using both N.W. and B.W. casing strings. This "double barrelled" casing-string method proved to be extremely effective in stabilizing the hole through to bedrock. Rock-core recovery was excellent, and is estimated to be 9?!!.
GEOLOGY OF THE BORLAND LAKE DEPOSIT
The silver mineralization occurs within two parallel, and roughly east-west striking silicified shear zones. The sheared zones lie in greywacke-type sediments, with the mineralization extending westwards along the structures from an ultramafic intrusive lying stratigraphically to the east. The mineralization consists of varying amounts of sulfide minerals, namely (in order of abundance) pyrite, pyrrhotite, argentite, galena, sphalerite and arsenopyrite. The total sulfide content does not usually exceed 10% with the sulfides occuring as irregular stringers, and disseminations along foliation and shear planes. Hanging-wall alteration occurs as a distinct zone exhibiting up to 10?; garnet porphyroblasts.
Diamond drilling has delineated both the north and south mineralized zones over a strike extent of approximately 1200 feet. The north zone exhibits an average width of approximately 7 feet, with the south zone showing an average width of 10.5 feet. Calculation of the grade-thickness ratio for the south zone suggests that the main body of silver mineralization (Block B) plunges to the southeast at 65 0 (Fig. #3) .
-6-
RESULTS OF THE 1986 DIAMOND DRILL PROGRAM
The purpose of the recent drill program was to test the down-plunge extension of the main zone of silver mineralization at Borland Lake; as well as test an area near to the surface where tonnage had not been delineated. Six drill holes were completed, each hole intersecting both the north and south mineralized shear zones (Fig.#4). The assay results from the six holes are as follows:
Footage ofHole f Section Departure Azmuth Dip Intersection (Ft)MBL 86-1 3+75E 4+25S 004 -50" 330.
409.MBL 86-2 5+25E 4+50S 004 -50 0 318.
MBL 86-3 3475E 5 + 2SS 004 -53" 453.528.
MBL 86-4 2-t25E 3 + 50S 004 -53" 332. 332.426.
MBL 86-5 1+75E 3+25S 004 -53 0 326.368.
MBL 86-6 0+05E 1+75S 004 -45" 176.
0 0
0
00
0 03
58
0
'-340 '-433
'-323
'-459 -533
'-337 '-344'-428
'-343'-376
'-196
.0'
.0'
.2'
. 0'
. 4 '
.4'
.3'
.3'
.0'
.7'
.3'
4 5
Assay
.1602
.51oz
5.3002 over 5
58
14 0.7
1413
19
.2402
.6302
.03oz 044oz.40oz
.50oz
.49oz
.2302over 20
212. 0 '-220 .0' 13 .95o2over 8.
247. 7 '-251 .7' 23 .38o2over 4 .
AgAg
Ag; .2'
Ac)Ag
Ag AuAg
Aq
Ag
Ag ;.3'
over over
10. 24.
0.1 3oz
overover
over overover
overover
6.05.4
5.4 12.2.0
16.7.9
0.0202
0 0
1
1
AU
it
3t
5'
f
'
Au
Ag; 0.055020'A9;
7'0.07o2
Au
Au
Drilling by Noranda Explorations prior to 1969 established Probable Ore Reserves of 244,493 tons at 8.27 ounces per ton silver and 0.02 ounces per ton gold. Noranda's exploration delineated the mineralization to the 250 foot level over a strike length of 1200 feet.
As a result of Massive's drill program, the Probable Ore Reserves now stand at 431,967 tons of 8.43 ounces per ton silver and 0,02 ounces per ton gold (Fig. #5).
Grade Block From To Tons Ag AuA B C
4+25W 2+75W 10,1250+25W 5+75E 383,1856+25E 8+25E 38,657
TOTALS 431,967
8.008.765.23
8.43 0.02
-7-
The greatest potential for additional reserves is at depth under Block B which has been tested to the 400 foot level only. Continuity of this block alone to the 1,000 foot level would effectively double the ore reserves. Other potential areas for additional tonnage are under Blocks A and C and along strike to the east from Block C.
CONCLUSION AND RECOMMENDATIONS
Massive Energy's 1986 drill program increased the Probable Ore Reserves of the Borland Lake deposit by 187,474 tons, to a total of 431,967 tons at 8.43 ounces per ton silver and 0.02 ounces per ton gold. Further drilling is definitely warranted as it has the potential of doubling the present tonnage outlined at Borland Lake .
It is recommended that an 8000 foot diamond drill program be undertaken to further define the silver deposit at Borland Lake. The program would be designed so as to delineate the main block of silver mineralization (Block B) down to a depth of 600 feet, as well as test on induced polarization anomaly as recommended and outlined by Excalibur Consultants Ltd. (J. Boniwell, 1986) . An expenditure of $350,000 is budgeted for this phase of exploration.
PROPOSED EXPLORATION PROGRAM
The proposed exploration program would best be carried out during the winter months, and would consist of the following:
- surveying of grid lines over the ice of Borland Lake and Solon Pond.- complete a V.L.F. electromagnetic survey using the broadcast fields of NLK, Seattle, Washington, and NSS, Annapolis, Maryland to better define E-W and N-S trending structures.
- diamond drill the targets outlined by Excalibur Consultants; 3 drill holes totalling 1250 feet are recommended.- diamond drilling of the main block of silver mineralization at Borland Lake, to delineate the mineralization to the 600 foot level; 7 holes totalling approximately 6750 feet.
The budget for the proposed program is as follows:
- Re-establish grid lines over the ice of Borland Lake and Solon Pond 51,000.00
- V.L.F. electromagnetic survey, two transmitting stations, on all lines, total of 25 line-miles x $90/mile 2,250.00
- Diamond drilling of the main block of silver mineralization at Borland Lake, and test targets outlined by Excalibur Consultants Ltd.; total of 8000 feet x $35/foot, includes mobilization/demobilization, moves, camp and support costs 280,000.00
- Analytical costs; 350 samples x 5 25/sa. 8 ,750.00
- Logging, supervision, report writing and drafting, all inclusive 15,000.00
- Consulting Fees, 10 days x ?4007day
- Fixed Wing Transportation
- Contingencies
4,000.00
20,000.00
19,000.00
Total Exploration Expenditures
September l, 1986 Toronto,Ontario
$350,000.00
n
Kenneth V/. Johnson B. Se, Project Geologist
LIST OF REFERENCE
Boniwell, J. B. 1986
Geophysical Investigations at Borland Lake Area, Red Lake Mining Division Ontario, Massive Energy Ltd. private report.
Bourne, D. A. 1985 Report on Borland Lake Property, Favourable Lake Area, Red Lake Mining Division, Massive Energy Ltd., private report.
Johnson, Ken 1985 Report on Massive Energy's "Borland Outlier" Property, Massive Energy Ltd., private report.
DIAMOND DRILL RECORD BUSH PILOT CORKMATION DC.
Massive Borland Lake498
NAME OF PROPERTY
HOLE NO. MBL 86-1______ LENGTH ^..LOCATION Borland Lake Grid- LATITUDE _____T!________ DEPARTURE
ELEVATION Lake.——————— AZIMUTH 004
4 + 25S
DIP -50"STARTED March 15, 1986 F IM ,^ HFn March 17, 1986
FOOTAGE
398498
DIP
43"430
AZIMUTH
004
004
FOOTAGE DIP AZIMUTH
Of l HOLE NO. O P ~-1 SHEET NO.
REMARKS casing pulled
LOGGED BY .. K. W. JohnsonFOOTAGE
FROM
0
176.0
176.6
181.0
182.7
?01 . 8
^kx
P
TO
176.0
176. 6
181.0
DESCRIPTION
Casing
Granite Boulder
Fine Grained Greywacke- very fine grained, black with moderatefoliation @ 50" to C/A; sporadic garnets exhibited
182.7
201 .8
205.0
in coarse porphyroblasts to 1/8 inch diameter.
Breccia Zone- annealled fault zone; large chloriticclasts in a fine grained micaceous matrix; tracepyrite.
Fine Grained Greywacke-as previous; C/A at 40" with occasionalinterbed of chloritic material.185.6-190.0: becomes more chloritic andbioti tif erous; tight drag folding evident; C/Ashallows to 10", trace pyrite on foliation planes.196.4-196.8: Pegmatite Dyke196.8-201.0: Greywacke; as previous withmoderate foliation at 40 0 to C/A; becomes somewhatbrecciated at 200*.201.0-201.8: Pegmatite.
Brecciated Greywacke-highly foliated at 50" to C/A with chloriticsections.204.0-204.3: quartz-carbonate vein at 30 0 to C/A; drusy quartz with trace euhedral pyrite.
SAMPLE
NO.
86008600
\S Utl PH - IDES
1 Tr2 Tr
FOOTAGEFROM
198. 0203.0
TO TOTAL
203. C208. (
5
5
ASSAYSAu Aa
i; S OZ/TON OZ/TON
i
T rT r
NilNil
DIAMOND DRILL RECORD NAME or pnopEBTY-Massive BorlandMOLE NO.
Lake86-1SHEET NO, .FOOTAGE
FftOM
205.0
218.1
219.2
223.3
224.0
227.7
229. 2
*
TO
218.1
219.2
223. 3
224.0
227.7
229.2
256. 0
DESCRIPTION
Medium Grained Greywacke-massive and biotitiferous with faintbedding foliation at 50 0 to C/A.209. 5~|
211. 8-212. 2jJ Porphyritic dyke; medium grainedwith foliated chloritic selvages, 3% fine grainedpyrite along foliation planes.- at 214.0 large garnet porphyroblastsare evident, up to 1/2 inch diameter.
Pegmatite Dyke- biotite phenocrysts.
Fine Grained Greywacke- weak bedding foliation with occassionalquartz veining up to 2 inches in width, with C/Aat 15"; folding evident at 220.0 feet, shallowangle at 10 0 to C/A.
Pegmatite Dyke
Siliceous Greywacke- moderate to strong foliation at 70" toC/A; up to 204 biotite on foliation planes.
Pegmatite Dyke- slight potassic alteration; very coarsegrained and megacrystic.
Siliceous Greywacke- as previous with moderate foliation at70" to C/A; breccia/debris flow evident at 233 to 236 feet; angular to subangular clasts evident in a siliceous and sericitic matrix. 243.0-256.0: trace to 14 disseminated pyrite; stringers and fracture fillings of pyrite at 60" to C/A.250.0: greywacke becomes garnetiferous
SAMPLE
NO.
8600 860C 8600 860C 9600
^ SUL^M,
IOCS
3 4 U 5 U 6 20 7 Tr
FOOTAOCMOM
238.0 243.0 248.0 t, 2 53. 256.0
TO
243.0 248.0 253.0 0 256 258.0
TOTAL
55 5
0 3 2
ASSAYSAu Aa^ -. O/ NX
T r T r T r Tr Tr
oi ton
Ni 1 Nil Nil Nil Nil
DIAMOND DRILL RECORD NAME OF PROPER-TV Massive Borland LakeHOLE NO. 86-1——————.——————— SHEET NO.______3
FOOTAGE
FROM
256.0
272.5
293.0
302.7
t
TO
272.5
293.0
302. 7
305.4
DESCRIPTION
with 24 disseminated garnet porphyroblasts; mediumgrained.253.6-254.2: sheared and siliceouszone with irregular stringers of massive pyrite.
Fine Grained Greywacke- moderate foliation at 60" to C/A;interbeds evident of more felsic greywacke;occasional porphyroblast of garnet up to 1/4 inchin diameter.
Siliceous Greywacke- moderate foliation with biotitemarking foliation planes in concentrations up to204; siliceous ground mass; foliation at 50" to C/Atrace to 14 pyrite in stringers and along fractureplanes .- pegmatite selvages at 282.0 and292.5.
Fine Grained Greywacke- massive to slightly bedded at 60" toC/A; trace pyrite associated with the siliceousinterbeds .298.0-298.6: broken Ground, faultgoujc.299. 4-299. 8
300.4; Pegmatite Selvage.niotitif erous Greywacke
- moderately siliceous with a strongfoliation, 254 biotite in medium grained aggregatesmarking foliation planes; strong foliation at 60"to C/A; 34 fine grained garnet porphyroblastsevident; 14 fine grained disseminated pyrite withoccasional stringer of pyrite.
SAMPLE
NO.
8600860086018601
MtH.'*, lOtS
8 Tr9 Tr0 Tr1 14
f QOTAGCmow
278.0283.0301 .0303.0
10
283. t288. (303. (306. (
TOTAL
5i 5
23
ASSAYSAu Aa
i 01 TO*
TrTrTrTr
oi row
Nil:NilNilNill
DIAMOND DRILL RECORD NAME OF PROPERTY.
HOLE NO.
Massive Borland LakeSHEET NO.FOOTAGE
FROM
305.4
320.0
344.0
f*
TO
320.0
344.0
356. 1
DESCRIPTION
Fine Grained Greywacke- interbedded sequence of mafic greywackesand siliceous greywackes; bedding at 60" to C/A.-318.3-318.4; Quartz-carbonate vein with massive pyrite mineralization; quartz-carbonateselvages; vein at 50" to C/A.
Siliceous Greywacke- moderate foliation; occasional shearedsection with associated silicification; mineralizedsections throughout; foliation at 60* to C/A;occasional stringers of pyrite proximal to mineral ized zones with stringers at 10" to 70" to C/A.330.5-330.1]331.0-331.6] Mineralized Zone with up to30% pyrite and cerargyrite(AgCl) in quartz gangue; hostgreywacke siliceous and shearc331.8-331.9: pyrite stringers; 40* pyrite.over 1/2 inch widths.332.0-332.5: Pegmatite.333.0-334.6: sheared and chloritized zonewith moderate silicificationand l i d isseminated galena/argentite.335.7-336.0: pegmatite.336.0-337.2: siliceous and seritized zonewith 5% pyrite associatedwith sericitic zones; foliat ion at 50" to C/A.339.2-339.4: quartz vein with 5* pyrite
at selvages; vein at 60 0 toC/A.
Sheared Zone -sheared and chloritized zone with strongbiotite alteration; strong foliation at 50" toC/A; trace pyrite.
SAMPLE
NO.
3601360136013601 8601
860186018601860286028602
d.
86028602
\ IULPN|
IOCS
)
3J5 40 i
7 Tr33 30312
3 Tr4 H
FOOT *GtfftDu
306.0311.3316.0.318.0 319.0
321.0326.0.330.0335.0340.0346.0
351.0356.0
TO
3ii.r316. C318. C319. C 321. C
326. C330. C335. C340. C346. (351. C
356. C363. C
foi*L
5. 34.72.01.0 2.0
5.04.05.05.06.05.0
5.07.0
1
ASSAYSAn Aa
*. Of TON
TrTrTrTrTr
TrTrTrTrTrTr
TrTr
b I TOO
.52NilNil.72Nil
NilNil
4.943.38Nil
I*'HNil
NilNil
DIAMOND DRILL RECORD NAME OF PROPERTY———
HOLE NO. -—————66-1
Massive Borland lakeSHEET N O..FOOTAGE
FROM
356.1
363.0
364.3
371.3
f
TO
363.0
364. 3
371.3
409.6
DESCRIPTION
352.6-353.0: pegmatite353.0-356.1: strongly chloritic andbiotitiferous zone with K pyrite and tracesphalerite in siliceous sections.
Siliceous Greywacke-highly siliceous and altered unit withmoderate foliation at 60" to C/A; strong sericitialteration evident in more siliceous sections.356.6-357.2
358.2: Pegmatite359.0-359.3
362.0: strongly sericitic.
Pegmatite Dyke
Siliceous greywacke-as previous; good interbedded sequenceof alteration mafic and siliceous greywacke.364.8-365.0367.6-368.0: Pegmatite
370.0
Sheared and Siliceous Greywacke- sheared and chloritic greywacke; somesections exhibit up to 31 medium grained garnets;sporadic stringers of pyrite at 60% to C/A;garnetiferous sections carry up to 2% finelydisseminated pyrite.376.4-377. 2377.5-378.0378.6-379.0: Pegmatite; slightly379.3-379.5 potassic382. 2-382.8
381.3-382.0: 2% pyrite in stringers383.6-384.4: chloritic zones; heavyshearing with strong biotite alteration; 2*
SAMPLE
WO.
:
3602J602
8602860286028603
x Juirn, 100
)
)
7j3D
FOOT AGETHOU
365.0368. 0
373.0378.0383.0388.0
TO
368. C373. (
378. C383. (388. C393. (
TOTAL
3.05.0
5.05.05.05.0
ASSAYSAn An
i -. 01 TON
TrTr
TrT rTrTi-
cti ro*
1
Nil jNil j
. 82
.481.00Nil
DIAMOND DRILL RECORD NAME OF
HOLE NO.
Massive Borland LakeR fi- 1 , SHEET NO.FOOTAGE
f ROM
409.6
419.3
' 423.6
f
TO
419.3
423.6
429.0
DESCRIPTION
hornblende?; C/A at 60".386.0-386.2388.3-389.1
390.0: pegmatite; white, slight390.6-391.2 potassic alteration at 389'.392.2393.0
395.5-396.3396.6-398.5: garnetiferous greywacke with404.5-406.0 medium grained porphyro-blasts of garnet; sericitic alteration associated with porphyroblastic texture; trace disseminated pyrite.
Mineralized Shear Zone-highly silicified greywacke, alteredwith average of 51 disseminated and stringerpyrite; cerargyrite evident associatedwith sulfide-rich zones; moderate biotitealteration evident along fracture planes.415.5-416.0: 10% disseminated pyrite andcerargyrite in 'clots' up to 1/4 inch diameter.
Sheared and Chloritic Greywacke-strongly foliated and chloritized zonewith strong biotite alteration; garnet porphyro-blasts evident at 421'; trace to 21 disseminatedpyrite and stringer pyrite; C/A at 50".
Mineralized Zone -3* pyrite/cerargyrite on average in rtisseminations and 'clots'; strong biotitealteration at 45" to C/A.
SAMPLE
NO.
i6031603 5603 J60336033603
8603 3603
t SUL"*f
me*
! Tr 3 Tr 1 5%i 10 !i Tr
7 34 J U
f OOTACEMO"
393.0398.0 403.0 409.0414.0419.0
423.0 428.0
TO
398.0403. C 409. C 414. C419. C423. C
428. ( 433. (
TOTAL
5.05.0 6.0 5.05.04.0
5.0 5.0
ASSAYSAu Aa
i i. 01. TOM
TrTr Tr .01TrTr
0. 04Tr
ot rov
Nil.90Nil
5.06"0.46)1.14
18.3'2.01
check
S.Si*W
18.0
DIAMOND DRILL RECORD NAME OFHOI F MO
Massive Borland Lake86-]
SHEET NO.FOOTAGE
f ROM
429.0
467.0
TO
467.0
471.7
498.0
DESCRIPTION
Siliceous Greywacke
- moderately to slightly sheared withfoliation at 60" to C/A; exhibits sporadic interbedof chloritic material, could be mafic volcanic orultrabasic.
429.2-429.5: 101 garnet porphyroblasts429.9-430.4: chloritic interbed.433.0: foliation becomesdominant at 55 0 to C/A; biotite shards evident.435.8-436.9: chloritic shear zone437.9-439.0: siliceous mineralizedzone with 3% disseminated pyrite.
441.0-441.5445.5
445.7-448.0: Pegmatite450.6-451.3456.3-456,9
460.6: chloritic breccia zone465.3-466.3: pegmatite
Siliceous Greywacke-as previous 483.0-488.0: siliceous sectionwith 21 pyrite; foliation at 60 0 to C/A.
End of Hole
J^ J^~^ w' ifl^^
Kenneth w. Johnson
SAMPLE
"0-
y
3603
8604 86048604
x suim, loci
) 31
0 Tr 1 Tr2 2%
FOOTAGEFflOM
437.0
473.0 478.0482.7
TO
440. C
478. ( 482.'488.1
10HL
3.0
5.0 4. 75.3
ASSAYSAn Aax v Of TON
Tr
Tr TrTr
01 TO*
4.17;
Nil NilNil
DIAMOND DRILL RECORD njst nurr COKKMATKM me.
NAME O F PROPERTY Massive Borland lakeHOLE NO.
LOCATION
LATITUDE
ELEVATIOI
STARTED
MBL ft S-Borl
L5+25Ei I.akpMarch 18,
2and l,
. L ENGTH — ^
ake Grid .
AZIMUTH C
1986 FINiSMEO
|Qft feet
4+50S*n4 oMarch 20,
DIP -^n 01986
FOOTAGE
300'498'
DIP
-4 2 o-37 0
AZIMUTH
004
004
FOOTAGE DIP AZIMUTHMBL
REMARKS Casing pulled
LOGGED BY Kenneth W. JohnsonFOOTAGE
FROM
0
137.0
138.6
149.5
11
TO
137.0
138.6
149.5
174.4
DESCRIPTION
Casing in Overburden
Broken Core; Boulder Material
Interbedded Greywacke Sequence
- fine to medium grained greywackesinterbedded with sericitic greywackes; moderatefoliation at 70 s to C/A; some of the more siliceoussections are highly garnetiferous.
Mineralized Garnetiferous Greywacke- moderately to strongly sheared and silicified with strong foliation at 50 0 to 60 0 to C/A; garnets are porphyroblastic and medium grained; trace to 11 pyrite in disseminations and stringers; stronger porphyroblastic texture indicative of strongest mineralized sections.
149.5-150.0: 2% pyrite in slightlygarnetiferous and siliceous greywacke; moderateshearing .
150.0-152.0: sheared and garnet iferous greywacke, moderate biotite alteration;trace disseminated pyrite; shearing at 60" to C/A.152.U-152.4: annealled f&ult gougewith 3* disseminated pyrite.152.4-153.2: garnetiferous grey wacke with H pyrite.153.2-154.6: fault gouge, partially
SAMPLE
NO.
860486048604 8604 8604 8604 8604 8605 8605
^1"
3 U4 5%5 4* 6 Tr 7 34 8 3 1 9 Tr 0 Tr 1 Tr
FOOTAGEFROM TO
1
149.0153.0158.0 163.0 166.0 168.0 173.0 178.0 183.0
TOTAL
153.0 4.0158.0163.0 166. C 168. C 173. C 178. C 183. C 188. C
5.0
5.0 3.0 2.0 5.0 5. 0 5. 0 5.0
ASSAYSAu Aa
^ S OZ/TON
TrTrTr Tr T r T r T r Tr T r
OZ/TON
NilNilNil Nil Nil Nil Nil Nil Nil
DIAMOND DRILL RECORD NAME OF PROPERTY. Massive ^Borland LakeHOLE NO. MBL 86-2
SHEET NO..FOOTAGE
FROM
174.4
178.2
"
TO
178.2
185.0
DESCRIPTION
annealled with thin quartz-carbonate stringers evidentin broken core, 5% to 1 01 pyrite at stringer selvages;at 154.1 large pyrite clast, rounded, are evident andare composed of 6(H pyrite.
154.6-158.5: garnetiferous greywackewith up to 2% disseminated pyrite.158.5-158.9: 4% pyrite in stringerswithin garnetiferous greywacke.158.9-166.0: garnetiferous greywackewith pegmatite selvages at 163 feet.166,0-171.8: Mineralized GarnetiferousGreywacke: 10% garnet porphyroblasts with up to 3% disseminated pyrite; strong foliation at 60" to C/A;strong biotite alteration.166.7-167.1: fault gouge with up to 401massive pyrite.171.8-173.3: potassic pegmatite dyke.173.3-174.4: 101 garnet porphyroblasts.
Potassic Pegmatite Dyke
-highly siliceous and megacrystic withtrace pyr i Le.
Mineralized Shear Zone
-heavy shearing and silicificationevident with pyrite mineralization up to 10?. over shortsections; shearing at 50" to C/A.180.2-181.7: quartz-rich section withup to 10* fine grained pyrite in irregular stringers,shearing at 50 0 to C/A.183.5-185.0: silicified and shearedgreywacke with 5% disseminated fine grained pyrite.
SAMPLE
NO.
!6051605 !605J605i6055605)605
* SULPM,
lOCi
3
t
t1
l
FOOTACtmow
188.0190.5 195.6198.2203.4208.4209.4
TO
190. 5(195.6 198.2]203.41208.4209.4218.0
rtmi
2.55. 1 2.65.25.01.08.6
ASSAYSAn An
\ 1 02 TOW
TrTr TrTrTrTrTr
01 TOW
NilNil NilNilNilNilNil
DIAMOND DRILL RECORD NAME OF
HOLE NO. MBL 66-2Massive Borland Lake
SHEET NO..FOOTAGE
FROM
185.0
195.8
198.0
i
205.6
206. 7
1208.0
TO
195.8
198.0
205.6
206.7
208.0
218.0
DESCRIPTION
Sheared and Siliceous Greywacke- moderately sheared and siliceous grey wacke with strong to moderate foliation at 50" to C /h;becomes garnetiferous at 191.0'192.0-194.0: garnetiferous section(10* .garnet porphyroblasts) with 11 stringer pyrite;sulfide-filled {pyrite) fault gouge at 192.8; vuggywith pyrite crystals.194.0-195.6: quartz vein with contactsat 50" to C/A; biotitiferous selvages.
Mineralized Garnetiferous Greywacke- 20% garnet porphyroblasts in abiotitiferous matrix; strong foliation at 70 0 to C/A;fine grained stringer pyrite in concentrations of 51on average.196.8-197.8: massive quartz-pyri tccarbonate vein; *W pyrite on average.
Interbedded Greywacke Sequence- interbedded sequence of fine grainedintermediate to felsic greywacke; good bedding at 60"to C/A.203.0-205.0: garnetiferous greywackesilicious with trace disseminated pyrite.
204.5: fractures at 10" to C/Awith trace pyrite.
Garnetiferous Greywacke Sequence- as previous; trace pyrite.
Interbedded Greywacke Sequence- interbedded greywacke sequence withbedding at 70" to C/A.
Garnetiferous Greywacke- garnet porphyroblasts dominate withhighly siliceous sections exhibiting trace to 1* pyrite
SAMPLE
*o. *SUl*Hr
ionFOOTAGE
moM TO TOTAL
ASSAYS
v 1 of row 01 TOM
1
DIAMOND DRILL RECORD NAME OF PROPERTY..—
MOLE NO. MBL 86-2Massive Borland Lake
SHEET NO. .FOOTAGE
rpOM
218.0
260. 3
270. 5
l 308.0
l
TO
260.3
270.5
308.0
319.5
DESCRIPTION
in irregular stringers.208.0-208.3: massive pyrite associatedwith quartz-carbonate stringer; same radiating crystalsof Marcasite; vuggy texture exhibits good cubic crystalssilver in colour.
Fine Grained Greywacke- fine grained greywacke with a moderatefoliation marked by biotite shards, becomes progressive]richer in biotite down-hole; foliation at 60" to C/A;some interbeds of felsic greywacke evident.221.2-222.3: fault gouge with quartz-carbonate stringers and massive pyrite mineralization;some foreign granitic material.226.7-227.7: pegmatite.
230.0: greywacke becomes rich inbiotite; strong foliation at 35" to C/A.236.0-236.5239.5-240.3: pegmatite dyke.248.5-249.0249.7-251.2
Pegmatite - some greywacke material interspersed
Greywacke- as previous with moderate to slightfoliation at 50" to C/A.273.4-274.2: pegmatite276.3-277.3: breccia zone with pyriteinfillings; up to 15* pyrite total.278.4-281.6: pegmatite breccia zone;2% pyrite along fractures at 281.0.302.8-303.2: pegmatite.
Garnetiferous Greywacke - heavily sheared section of greywackewith 5% garnet porphyroblasts , strong foliation at 60"
SAMPLE
NO.
1
y3605
8COC
8606 860(860C
* mi*-,IDtS
9
0
1 23
FOOTAGEnou
220.3
276.0
308.0 313.0318.0
TO
222.4
278.
313. 318.323.
TOTAL
2.1
i 2.0
1 5.0 ) 5.0i 5.2
ASSAYSAu Aa
i \ 01 TD*
Tr
T r
0. 01 0.010.13
(It 10-
Nil
Ni 1
Nil Nil
5. 3 0
DIAMOND DRILL RECORD NAME OFHOLE NO. MBL 86-2 .
Massive Borland LakeSHEET NO.FOOTAGE
rftOM
319.5
323. 3
1
TO
323.3
362.8
DESCRIPTION
to C /A: up to 5% pyrite in more garnet-rich sections,overall 2% pyrite; dragfolding evident at 318.0.313.0: quartz-carbonate vein with 21pyrite.
Fine Grained Greywacke- as previous; slightly garnetiferouswith slight foliation and/or bedding at 50' to C/A.
Garnetiferous Greywacke- slightly garnetiferous at 323.3 andbecomes progressively more so down hole; trace to l istringer pyrite associated with the garnet zones.326.0-326.2: stringer of pyrite-galona-argentitc in concentrations of 5%.327.2-328.0: pegmatite.328. 0-328. 5: quartz-carbonate-pyritevein with trace argentite.
329.5: galena-argentite stringer;1/4 inch in width.330.6331.5: quartz-carbonate-pyrite332.5 stringers at 50" to C/A.333.4
331.5332.6: quartz-carbonate-pyrite337.6 stringers at 50" to C/A.338.6
336.6-336.9: potassic pegmatite.340.8-341.6
329.0-330.0: 2% stringer pyrite insheared greywacke; quartz-biotite-garnet matrix; strongfoliation at 50 0 to C/A.
SAMPLE
NO.
860i860i8601860i860'
860860
IOCS
45678
90
FOOTAGEFftOu
323.2328.4332.9338.2343.3
348.7352.0
TO
328.4332.9338.2343.3348.7
352.0357.0
TOTAL
5.24.55.34.15.4
4. 75.0
ASSAYSAn Aai or rot
TTTrTrTrTr
TrTr
01 TON
NilNilNilNilNil
NilNil
j
DIAMOND DRILL RECORD NAME OF PROPERTY.
HOLE NO. M B L 86-2
Massive Borland LakeSHEET NO..FOOTAGE
r ROM
362.8
378. 3
U17.8
f
TO
378.3
417.8
429.2
DESCRIPTION
341.6-357.0: 4% disseminated pyrite,trace argentite in highly siliceous and garnetiferousgreywacke; strong foliation at 40" to C/A; good sulfidestringers associated with quartz-carbonate stringers.357.0: fault gouge; broken core.357.6-362.8: heavy shearing; strongbiotite alteration; shear selvage.
Siliceous Greywacke- medium grained siliceous greywackewith occasional interbed of mafic greywacke; foliationat 55" to C/A.
376.3: quartz-carbonate-pyritestringer at 55" to C/A.
Biotitiferous Greywacke- garnetiferous at top of section becomirprogressively more micacious down hole; at 381.0 becomesvery schistose with strong schistosity at 60" to C/A;trace disseminated pyrite along foliation planes.387.0-388.2: sheared and chloritizedsection; could be mafic intrusive.388.2-389.0: siliceous section.389.0-390.6: fault gouge.391.6-393.9: sericitic greywacke.moderately sheared and siliceous with clots of sericiticmica; very fine grained.399.4-401.2: potassic pegmatite dyke.404. 7-405.1
411.3-417.8: sheared and siliceous zonewith up Lo 2* pyrite in disseminations and irregularstringers; moderate foliation at 60 0 to C/A.
Sheared Mafic Intrusive- highly sheared and chloritized andbioti tif erous sections with 2% stringer and ^isseminatec
SAMPLE
NO.
J
86078607860786078607
X iUl'K,
IOC1
1234 2 1,3
FOOTAGEr.ou
407.0412.3417.0420. 0429. 3
TO
412.:417. (420. (429. .434.
TOTAL
3.34. 73.09. 35.0
ASSAYSAn An
\ 01 TOW
TrT rT rT rT r
01 TOD
1
i
i
NiltillNilNilNil
DIAMOND DRILL RECORD NAME OF Massive Borland LakeHOL E NO MBL 86-2 SHEET NO.FOOTAGE
FROM
129.2
K
TO
98.0
498.0
DESCRIPTION
pyrite; weak foliation at 70" to C/A; appears massive,slightly carbonated; probably sheared peridotite,slightly talcose.429.0: galena-argentite stringer,1 inch in width.
Siliceous Greywacke- massive and fine grained siliceousgreywacke; exhibits fine grained shards of biotite at2%; trace pyrite in occasional stringers.432.6-432.9: pegmatite.447.1-448.1: breccia zone; broken core- at 450.0 thin fractures filled withquartz are evident; dominantly at 50 0 to C/A.
End of Hole
Kenneth W. 'johnson
SAMPLE
MO. * SUl'M,
IOCSFOOT AGt
MOM TO TOTIl
ASSAYS
v1 Of TON 01 fOM
!
l/)t
MJSH MLOT COftrOftATION INC.DIAMOND DRILL RECORDNAME OF PROPERTY Massive Borland Lakeun . r ^ M BL 8 6 ~ 3 ,E N r.TM fidfi Feet, NATION Borland Lake Grid . . .ELEVATION Lake AZIMUTH 004" DIP -5.1"
M^.v-^.1-, -51 IQRf, Mjar-^h 7/1 1QRK
FOOTAGE
426600700
ppv
DIP
-43 0-38 0-34 0
AZIMUTH
004
FOOTAGE DIP AZIMUTHj Rfi-
REMARKS - . Csiai n g Pill 1 ort
LOCOED BY ,Kenneth W. Johnr-.qnFOOTAGE
FROM
0
236.0
238.2
238.8
240.4
252. 4
276.0
280. 8
T*
TO
236.0
238.2
238.8
240.4
252.4
276.0
280.8
294.0
DESCRIPTION
Casing in Overburden
Boulders; granitic and sedimentary in origin.Greywacke
Potassic Pegmatite Dyke
Siliceous Greywacke - highly siliceous greywacke with moderate foliation at 70" to C/A; medium grained with clasticappearance. 250.5-252.4; potassic pegmatite dyke.
Sheared Zone- highly schistose and micaceous zone; primary textures not readily observable; strong schistosity at 60"; some sections pegmatite; all sections very soft and friable (fault zone?).
Siliceous Greywacke - as previous; becomes sheared at 278.0.
Mafic Intrusive- sheared and foliated mafic intrusivegabbro, or mafic volcanic; exhibits some intercalate greywacke sections; shearing evident at 60 0 to C/A; chloritic and biotitif erous.
SAMPLE
NO.
1
WTFOOTAGE
FROM TO TOTAL
ASSAYS
V x 02/TON OZ/TON
DIAMOND DRILL RECORD NAME OF PROPERTY. Massive Borland LakeMBL 86-3
SHEET NO. .FOOTAGE
f ROM
294.0
299.1
322.8
344. 3
T
to
299.1
322.8
344.3
356.0
DESCRIPTION
Siliceous Greywacke- as previous
Sheared Mafic Intrusive- appears gabbroic; moderately sheared tomassive in some sections.309.8-315.6: becomes porphyritic with 2%feldspar porphyroblasts.320.0-322.8: white pegmatite.
Greywacke- moderately foliated and siliceous,foliation at 70" to C /h; some interspersed gabbroicsections, foliated and sheared greywacke bounds thegabbro.325.0-326.0: quartz vein, bull white at60" to C/A.- becomes sheared and moderatelybiotitifcrous at 336.0 feet; foliation at 70 0 to C/A.338.2: quartz-carbonate stringer at342.6 50 0 to C/A, with pyrite at
selvages.
Mineralized Greywacke- sheared and siliceous greywacke withmoderate foliation at 70 0 to C/A; up to 3% stringerpyrite associated with the more siliceous sections;strongly bioti tif erous with gneissic-like bands ofalternating siliceous and biotite-rich sections.347.2-349.3: game tif erous-siliceousgreywacke; porphyroblasts of garnet up to 1/4 inchin diameter oriented along foliation planes inconcentrations up to 54; l i d isseminated pyriteassociated.349.5-352.7: 34 pyrite in stringers at 10to 60" to C/A; associated with siliceous zones;trace AgCl.
SAMPLE
NO.
8607860786078607860886088608
X SUL'H,
toes
6789012
FOOTAGEmow
336.0341.0346.0351.2356.0361 .0366.5
ID
341.!346. (351.:356.1361.1366.!371.!
101*1
5.05.05.24. 85. 05. 55.0
7^5AVS Agi \ 01 TON
T rTrT rTrT rT rTr
(it TON
NilNilNilNilNilNilMi 1
DIAMOND DRILL RECORD NAME OFHOI F MO MBL 86-3
Massive Borland LakeSHEET NO.
FOOTAGE
FROM
356.0
358.0
364.5
369.4
ItT
TO
358.0
364.5
369.4
444.3
DESCRIPTION
354.0-356.0: pyrite in irregu lar stringeBrecciated Greywacke
- siliceous fragments in a medium grainedmassive matrix.
Siliceous Greywacke- as previous; slight foliation at 70" toC/A.
Mineralized Greywacke- as previous with 21 pyrite stringerswith biotite-rich sections.
366.5: trace AgCl
Siliceous Greywacke- moderately foliated at 60" to C/A; biotishards mark foliation planes.
374.6376.6: trace pyrite associated with384.4 siliceous zones.387.2
390.6-392.0: sheared and siliceous zone;strong foliation at 50 C to C/A; quartz vein at391.5-392.0; trace pyrite.392.0-393.8: slightly garnetiferoussection; in biotite-rich and siliceous zone; 2*stringer pyrite associated with siliceous zones.402.5
403.7: fault gojge.404.9
407.0-408. B412.0: sericitic alteration with412.6 porphyritic-serici tic in413.4-413.8 disseminations.
SAMPLE
NO.
S
i608i608!6085608S608)608 J6083609
:O
\ SUL**( lOt)
3i
i
)1
3 3)
FOOTAcernoM
386.5391.5396.5401.5406.5411.4 416.5421.4
ro
391.5396.5401.5406.5411.4416.5 421.4425.9
TOTAL
5.05.05.05.04. 95. 1 4.94.5
A KV YS Ag-. \ 01 TON
TrTrTrTrTrTr TrTr
ffi T OM
NilNilNilNilNil \Nil NilNil
DIAMOND DRILL RECORD NAME OF PROPERTY- Massive Borland LakeHOLE NO. MBL 86-3
SHEET NO..FOOTAGE
FROM
444.3
451.0
468.5
487. 8
It• 01.1
TO
451.0
468.5
487.8
501.1
504.9
DESCRIPTION
418.8-421.0: siliceous zone with slightbiotite alteraion, up to 3% disseminated pyriteassociated with siliceous sections.442.3-444.3: 2% pyrite in stringers assoc iated with siliceous sections.
White Pegmatite- fine to medium grained dyke; very siliceousno mineralization noted.
Mineralized Greywacke - siliceous section with moderate shearingevident; trace biotite alteration; 5% stringerpyrite evident in siliceous sections trace to J.%Marcaskic pyrite.458.0-459.0: 5% pyrite in siliceous andsheared section; H galona-argentite evident.
Siliceous Greywacke- very fine grained and siliceous with slightfoliation at 70 0 to C/A.468. 5-471 . 0471.4-472.6: shear zone; chloritic and473.5-474.0 siliceous
478.0-478.5: ground core.480.8-481.0: white pegmatite.
Pegmatite Dyke- sheared and slightly potassic.491.2-492.8: greywacke
498.0: ground core.498.0-499.5: sheared and potassic zone withtrace to H pyrite on fractures.
Sheared Zone- highly chloritic and bioti bif crous with
*4O.
!609
8609 860986098609
t StHPH, IOCS
.
2 313
SAMPLE
F~OOT~AGSF*OM
441.2
453.0 456.0459.0464.0
10
446. 0
456. C 459. (464. (468. i
rOTAL
4. 8
3.0 3. 05.04. 8
i
ASSAYS————— . ______ a 11 ftfi ____ _
i or 'ON
Tr
Tr 0.02TrTr
—— —3 ———
01 row
Nil
Nil 9.84NilNil
DIAMOND DRILL RECORD NAME OF pROPERTv—^Jlaaal^ii.^Borlan.d Lake HDI F no M BI. B6-3 sneer NO.FOOTAGE
FfiOM
504.9
518.0
533.1
IO
518.0
533.1
579.5
DESCRIPTION
strong foliation at 35" to C/A.
Siliceous Shear Zone- sheared and silicified zone with bandingof silica-rich sections; biotite shards mark slightfoliation at 70 0 to C/A; trace pyrite noted.510.4; stringer of Marcasiticpyrite at 70" to C/A.
514.0: trace argentite along fract ure plane.
Garnetiferous Greywacke- siliceous and sheared greywacke withgarnetiferous sections throughout; porphyroblastictexture, slight to moderate foliation at 70" to C/A.531.5-533.1: potassic pegmatite,sericitic alteration along fractures.
Mineralized Greywacke- siliceous and sheared section with up tcS 1* pyrite in stringers and disseminations; moderatebiotite alteration associated with sheared sections.trace Lo 3% argentite-galena over short, shearedsections; foliation at 65 0 to C/A.535.1-537.0: stringer and disseminatedargentite-galena; in concentrations to 3%.539.0-540.0: 3% pyrite stringers ingarnetiferous greywacke.548.9-549.9: 10*. pyrite stringers ingarnetiferous greywacke; 31 Cerargyrite (AgCl)associated with sulfide-rich sections.
550.7: trace argentite.562.0-563.5: 10i irregular pyritestringers with 5% cerargyrite associated.566.7: quartz-carbonate stringerwith l Ot, pyrite.
SAMPLE
NO.
!60956095609560956108610861086108610
8610861C861C861C861086118611
tlUl'H,
IOCS
)
7
i
)
)
1
234
5678901
FOOT AGEmoM
504.5508.0513.0528.0533.4535.0538.0543.0548.0
553.0558.0563.2568.0573.0577.0582.0
TO
508. 0513.0518.0533.4535.0538. (543. (548. (553. (
roT*t
3.55.05.05.41.63.05.05.0
i 5.0
558.6 5.0563. i 5.2568.6 4.8573.? 5.0577. (j) 4.0582.587.
l 5.0l 5.0
ASSAVSAll An
•; 01 TO*
TrTrTr
0.03TrTrTr0.030.05
0.03TrTrTr
0.04Tr
0. 02
6i 10*
NilNilNil
8. 63Nil1.13Nil
1.71Nil
5.004
2.82Nil,NilNil:
2. 93|Nil]Nil
o'
DIAMOND DRILL RECORD NAME or PROPERTY Massive Borland Lake KOI F MO MRT. 86-3_______ SHEET NO,_
FOOTAGE
f ROM
579.5
650 .4
656.3
684 .7
692.7
r
TO
650.4
656.3
684.7
692. 7
698.0
698.0
DESCRIPTION
566.8-572.0: sheared and chloritic section;moderate to strong foliation at 70 0 to C /h.572.0-576.7: siliceous mineralized greywackeweak foliation development exhibited; trace to 11biotite shards; trace to 11 stringer and disseminatedargentite associated with siliceous sections. 574.4-575.2; 2% argentite along fractureplanes.576.1-579.5: sheared and chloritic greywackemoderate to strong foliation at 40" to C /h; biotite-rich partings mark foliation planes.
Siliceous Greywacke- moderately sheared and silicified greywackeslight foliation at 50" to C /h; trace pyrite on fracturplanes.579.9-580.6: siliceous zone.595.6-596.4
599.6-600.4: quartz veins at 50".631.0: fractures at 50 0 .
White Pegmatite
Fine Grained Greywacke- foliation at 65" to C/h.
White Pegmatite- interf ingered greywacke evident.
Siliceous Greywacke- foliation at 65 0 to C /h.
End of Hole.
Kenneth W. Johnson
MO.
!
a SULPX,SAMPLE
FOOTAOC
ASSAYS
-, •V 01 TO* fit TDK
1
DIAMOND DRILL RECORDNAME OF PROPEHTV Massive Borland Lake——————MSL 86-4 .,^,. u 498 Feet
KISH mor couoiuTtON INC.
HOLE NO.
LOCATION ROT" LATITUDE L2+25E ELEVATION Lake
LENGTH
e GridDEPARTURE
. AZIMUTH
3 + 50S
STARTED,March 24, 1986 FINISHED,March 26. 1986
FOOTAGE
363'498'
DIP
450
42"
AZIMUTH
004
FOOTAGE DIP AZIMUTHHOLE NO. fifi-4 SHEET NO. .
Casing pulledREMARKS.
LOGGED BY Kenneth W. JohnsorxFOOTAGE
FROM
0
159.0
195.9
f
TO
159.0
195.9
210.5
DESCRIPTION
Casing in Overburden
Greywacke- moderate foliation at 50" to C/A;moderately biotitif erous and medium grained.
169.6: quatrz vein with sericitealteration along selvages; strong schistosity at45 0 to C/A.169,7-171.4; quartz-carbonate vein at40" to C/A; exhibits silicified selvages; nomineralization noted.172.6-174.3: sheared and silicified176.0-177.0: section with epidote?alteration; trace pyrite sporadic garnets.
179.8180.8-182.2
183.0: sheared and garnetiferous185.4 zone with moderate foliatio;188.0-188.7 at 40" to C/A.189.0
- at 191.0 greywacke becomes siliceous;strong shearing evident at 193.0.
Mafic Intrusive- moderately to highly shearedSerpentinized Peridotite; talc-silicate alterationalong fracture planes; highly biotite-rich withbiotite porphyroblasts marking foliation planesat 50" to C/A; moderately to highly chloritic;hematite noted along fractures at 90" to C/A.
SAMPLE
NO. SULPH IDES
FOOTAGEFROM TO TOTAL
ASSAYS
X ? OZ/TON OZ/TON
i
DIAMOND DRILL RECORD NAME OF PROPERTY.
nr*i f urt O D—M
Massive Borland Lake
SHEET NO. .FOOTAGE
FROM
210.5
227.9
234.8
241. 6
"
J248.2
TO
227.9
234.8
241.6
248.2
281.8
DESCRIPTION
Greywacke- fine grained biotite shards markfoliation planes at 60" to C/A.
210.5-211.1: sheared greywacke withtrace pyrite along shear planes.212.0-212.9: sheared and chloriticzone.212.9-227.9: biotitif erous greywacke,strongly biotite-rich with strong foliation at 60" toC/A.215.0-215.2216.3-216.7: White Pegmatite217.0-217.5218.0-218.3
Siliceous Greywacke- fine grained with trace pyrite alongfracture planes; moderate biotite phenocrysts markfoliation at 60 0 to C/A.231.0-231.2: garnet phenocrysts evident- pyrite stringer with carbonateselvages evident at 230.9 feet.230.9-234.8: trace pyrite alongfoliation planes.
Sheared Greywacke- moderate shearing a t 5 0" to C/A; biotashards mark foliation planes.
Biotitif erous Greywacke- strongly biotitif crous in sectionswith siliceous zones throughout; trace stringer pyrite;strong foliation at SO 0 to C/A,245.3-246.0: Potassic Pegmatite Dyke.
Siliceous Greywacke- moderately to highly siliceous grey-
SAMPLE
NO.
86118611861186118611
to
\ 1ULPM, IDf)
234)
6
FOOTA06FROM
228.0232.7238.0243.0248.0
TO
232.'238. (243.1248. (253. (
TOT*L
4.75.35.05.05.0
tfu* 1' 5 Ag-. -. 01. TON
TrTrTrTrTr
01 TOM
1
NilNilNilNilNil
DIAMOND DRILL RECORD NAME OF PROPERTY. Massive Borland LakeHOLE NO. MSL 86-4
SHEET no..FOOTAGE
FROM
281.8
288.2
|1329.5
TO
288. 2
329.5
331.8
DESCRIPTION
wacke with slight foliation evident , marked bydisseminated biotite shards; foliation at SO 0 toC/A.253.6-253.9: White Pegmatite.259.9-260.5: 44 stringer pyrite insheared biotitif erous zone.260.5-261.9: Potassic Pegmatite.262.5-263.5: siliceous breccia zone.267.0: 2% stringer pyrite at 40 0to C/A in sheared and biotite-rich section.267.7-268.0: White Pegmatite268.5-268.9
273.5: quartz-carbonate stringerat 40" to C/A with 54 euhedral pyrite crystals.274.4-281.8: sheared and garnetiferousgreywacke with 14 stringer pyrite associated withbiotite-rich sections; moderate to strong foliationat 50 0 to C/A; sporadic garnets evident, porphyro blastic up to 1/4 inch in diameter.
Interbedded Greywacke Sequence- interbedded mafic and chloritic grey wacke sequence; remnant bedding at 50 0 to C/A.Siliceous and Sheared Greywacke
- some garnetiferous sections; quartzveining at 40" to C/A at 292.0 feet.- becomes massive and very siliceous at300 feet.322.7-323.5: Pegmatite selvage.
327.2: Pegmatite.328,0-328.3328.4-328.9: biotitif erous and sheared;strong foliation at 60 0 to C/A.
Potassic Pegmatite Dyke- megacrystic
SAMPLE
MO.
5611
)611
t SULPN,
IOCS
t
f DOT ACEfftOM
258.0
273.0
TO
260.0
279.1
TOIAl
2.6
6.1
A!SQVS Aq-.
: h
-. 01. TOM
T r
Tr
01 TON
Nil
Nil
DIAMOND DRILL RECORD NAME OF PROPER-TV Massive Borland Lake HOLE NO. MSL 86-4————— SHEET NO. .
FOOTAGE
FROM
331.8
344. 0
347.0
356.0
378.9
|1
TO
344.0
347.0
356,0
378.9
426.2
DESCRIPTION
Mineralized Greywacke- highly sheared and siliceous zonewith up to 5ri stringer pyrite and 31 galena-argentite in irregular disseminations, foliationand shearing at 55" to C/A; some chloritic shearzones within section carry trace of AgS.331.6-333.4: 5% pyrite in thinstringers at 55" to C/A.334.5-336.7: chloritic zone with 3*istringer pyrite and trace, argentite; somewhatbrecciated.337.6-343.0: up to 3% galena-argentite associated with pyrite-rich and siliceoussections.
Brecciated Greywacke.
Siliceous Greywacke- siliceous greywacke which becomesgarnetiferous at 355.0 feet.
Garnetiferous Greywacke- highly garnetiferous in sections;matrix of siliceous greywacke; trace pyrite inmatrix .361.6-363.2: 21 pyrite in stringersalong foliation planes, in sheared and silicifiedsections; foliation at 50" to C/A.364.0-364.8: 10% stringer pyritein irregular clots and along foliation planes.367.0-369.1: White Pegmatite.
Greywacke- medium grained and foliated at 60"to C/A; slightly garnetiferous in sections; tracedisseminated and stringer pyrite.386.6-387.0: Pegmatite
387.5
SAMPLE
NO.
86118612861286128612
8612861286128612
t SULFX,
1015
}
DJ23
4567
POOTACErftOM
327.0332.0337.4341.6344.3
359. 7365.0369.9373. 2
TO
332. C337.'341. f344.348. C
305.369.373.379.
TOTAL
5.05.44.22.73.7
5. 34.9
23.3) 5 . 8
ASSAYSAu Aa-. or TON
Tr0.040.060.03Tr
T rTrT rT r
01 TON
Nil14.0NilNilNil
|
NilNil
1 . 500. 90
DIAMOND DRILL RECORD NAME OF PROPERTY. MH, r.o MSL 86-4
Massive Borland LakeSHEET NO..
FOOTAGE
F HDM
426.2
437 .4
462.5
|n1
TO
437.4
462.5
498.0
498.0
DESCRIPTION
390.0-390.8: massive pyrite (40%)with quartz gangue; sheared selvages at 60" to C/A.396.0: clay seam.
404.0-405.7: White Pegmatite.413.1-414.2: brecciated greywackewith trace pyrite.421.3: pegmatite.
Mineralized Greywacke- sheared and silicified zone with upto 10% galena-argentite over short sections (6 inchesaverage) ; l i d isseminated pyrite associated with thesiliceous sections.427.0-427.8: 1 QI galena-argentite inirregular stringers, 5% pyrite stringers associated.
Greywacke- slightly sheared and chloritizedsections exhibit good foliation at 60" to C/A;most sections medium grained and massive.442.0-442.4: quartz veins withbiotitc-rich selvages at 50 0 to C/A.444.5-445.0: White Pegmatite.446.3-447.1
458.0-458.9: brecciated greywacke461.0-462.5
Siliceous Greywacke- massive to bedded greywacke withbedding and slight foliation at 50" to C/A.489.2-489.6: White Pegmatite.
End of Hole.
/(U L ' V—Kenneth W'. JohnsonMarch 27, 1986
SAMPLE
NO.
5612
8612861386138613
t SIH'N, rOC!
3 401
3D 10!1p
FOOTAGEMOM
389.:
424.0426.
428.3431.0
10
392.
426.21 428.431. C434. C
TOTAL
0 2.9
2.33 2.0
2. 73.0
AWS Ag^
F
\ 01- TOM
Tr
T r0.01TrT r
t,l I0i
Nil
Nil7. 40Nil
0. 84
DIAMOND DRILL RECORD ipc- KISH fUOT COXKXtATlON INC.
NAME OF PROPERTY
HOLE NO. MBL P6-
LOC A T ION
LATITUDE
ELEVATION
Massive Energy Limited500 feet
Borland Lake Grid1 + 75E
DEPARTURE
.AZIMUTH ^.
3+24SQQ4
26, 1986 March 28, 1986-53
FOOTAGE
dollar300
500
DIP
-53-48
-46
AZIMUTH
004
FOOTAGE DIP AZIMUTH
REMARKS.
LOGGED OY Peter EitutisFOOTAGE
F ROM
0
141.2
159. 3
1
TO
141.2
159.3
DESCRIPTION
Casing In Clay Overburden
Greywacke- moderately foliated with foliation
rich in biotite shards.- foliation at 40" to C/A.
184.5
148.0-148.2: Pegmatite - slightly155.0-155.5 potassic.
158.0: Ground core158.9: small fractures with
talc S carbonatealteration.
Siliceous Fine Grained Greywacke- slight foliation at 40" to C/A- foliation has trace PYRITE166.5-168.0: sheared pegmatite
with slight greenishquartz .
172.7-173.3: sheared greywacke withslight garnets.some chloritic alterataround garnets.stringers at quartz-carbonate with tracepyrite.
175.0-175.6: q tz-carbonate vein at15 0 to C/A.
SAMPLE
NO.
on
*SULPH IDES
FOOTAGEFROM TO
i
TOTAL
ASSAYS
* * OZ/TON OZ/TON
DIAMOND DRILL RECORD NAME OF Massive Energy Limitednni F NO MSL 86-5 SHEET NO.
FOOTAGE
r ROM
184.5
187.2
j
1
TO
187.2
209.0
DESCRIPTION
176.0-176.4: garnets in greywacke-176.4-178.2 slight fractures at15 0 to C/A.
-filled with chloriticcarbonate alteration
-qtz S pyrite crystalswell developed.
178.2-179.8; greywacke withincreased biotitealong foliation.
179.2-181.1: SHEARED PEGMATITE181.1-184.5: zones of garnets andchlorite- carbonatestringers in siliceoigreywacke.
Siliceous Sheared Greywacke- has quartz phenocrysts and somechloritic alteration.- small stringers rich in talc at20" to C/A
187.2: lost core
Mafic Intrusion- highly to moderately shearedperidotite- talc-silicate along fractureplanes- some carbonate alteration also- biotite porphyroblas ts alongfoliation at 40" to C/A.187.2-189.8: chloritic alteration206.0-209.0 along contact of
mafic intrusion.
209.0-211.0: PEGMATITE
SAMPLE
MO.
t
S
x iuon tIOCS
FOOTACfrnoM TO TOT*l.
j
ASSAYS
\ Ot- TON til TON
j
l
l
DIAMOND DRILL RECORD N AM E OF PROP t K i v- ... .Ma s s i y c Energy Limited HOUe NO MBL 86-5 iMtf-T NO.,TOO
rwOM
209.0
229. 3
r AGE
TO
229.3
258.0
OESCWTION
Greywacke - fine grained biotite shards alongfoliation planes at 40" to C/h- trace pyrite along foliation- chlorite alteration spotty and parall(to foliation218.0-218.6: broken core
- carbonate alteration alonefractures parallel tofoliation
220.3-226.0: increasing biotite contenmarking foliation planes
223.1-223.9: GREY PEGMATITE226.0-229.3: SHEARED CHLORITIC GREY
WACKE-carbonate alteration alonifractures at 35 0 to C/A.
-chloritic alterationparallel to foliation at25 0 to C/A.
Siliceous Greywacke- fine grained with trace pyrite alongfoliat ion230.7-233.5: biotite along foliation
28" to C/A233.5: carbonate stringers.
233.5-234. 1234.5: garnets with increased235.4 biotite along foliation
237.0-238.9 planes.-garnets about 1/B" indiameter.
238.9-239.1: large garnets 1/4" Lo3/8" in diameter
HO
1
\ W l *H
'DES
S A M f ' i
f SQw
rF OOT A T, f
'0 101*1
ASSAYS
01 - tQn 01 t ot
\
\
j;'
DIAMOND DRILL RECORD NAME Of PHOPFRTY
,,mFNO MSL 86-5Massiye _Energy^L imited___ . - . our c t NO ——-————roo T A c; f:
,HO- TODESCRIPTION
-foliation at 30 0 to C /h-strong biotite association withthe foliation.239.6-241.5: stringers of quartz-carbonate247.0-247.3: quartz vein
247.7-248.5: PEGMATITE with 3% biotitephenocrysts248.5-258.0: becoming more siliceous withquartz phenocrysts.
250.0-253.0: slightly mineralized-34 pyrite-trace cerargyrite256.0-256.9: garnets with pyrite stringersparallel to foliation at 60"to C/A.
263.7-264.3: PEGMATITE - slightly potassic265.0: trace pyrite along foliation265.5-265.6: quartz vein with trace pyriteand small garnets.267.6-267.8: quartz- feldspar vein268.0
269.6: talc-chlori to alteration inthin vein.
-vein parallel to foliation at60 0 to C/A
274.2: CARBONATE STRINGER with tracepyrite parallel to foliationat 60" to C/A
-also fracture (at right anglesto foliation) filled withquar t z- carbonate
274.2-279.0: carbonate alteration in fracturiparallel to foliation277.5: quartz stringer
SAMPUE
HO.
8613
8613
!S
X Sui^w
.00
3
4
FOOTAGCrftOM
248.4
252.9
TO
252. ̂
258. (
TotM
4.5
5. 1
ASSAYS ,AU Aq-. O l to*
Tr
Tr
01 TOM
Nil
Nil
|
1
DIAMOND DRILL RECORD NAME OF PROPERTY.
HOLE n o. .-MBL 86-5
Massive Energy Limited
SMEE T NO..TOOT AGE
r BOM
323.5
326.9
339.7
341.7
358.8
TO
326.9
339.7
341.7
358.8
362.2
DESCRIPTION
322.2-323.5: PEGMATITE
Biotite Greywacke - trace pyrite
Mineralized Sheared Greywacke - 104 pyrite, trace agrentite- sections with garnets and chloritic altera tion- talc and chloritic fractures parallel tofoliation- foliation at 70 0 to C/A330.7-338.0: garnetiferous - more siliceous
- trace argentite- pyrite parallel to foliation@ 70 0 to C/A
339.0: trace argentite
Biotite Greywacke- foliation at 70" to C/A
Siliceous Greywacke- phenocrysts at quartz - trace pyrite along foliation @ 70 0 to C/A- zones of chlorite alteration along fract ures parallel to foliation
347.7: quartz carbonate alterationin fractures
349.0-350.0: garnets 1/8" in diameter -25i350.0-358.8: biotite shards along foliationat 60" to C/A
- trace pyrite- trace garnets at 358.0 feet.
Pegmatite - slightly potassic 360.8-361.0: chloritic biotite grey-361.4-361.9 wacke with foliation at
70" to C/A
SAMPLE
MO
S613
J613 5613
8614
8614
a iui'H toe s
j
i )
0
1
FOOTAGEfVOw
323.8
326.5 331.9
338.0
343.0
10
326.5
331.9 338.0
343. (
348. (
'01*1
2.7
5.4 6.1
5.0
15.0
A!Su- YS Ag•\ of. lot
Nil
0.03Tr
0.03
Tr
b t TO*
Tr
17.33 14.6*
11. 2 f,
Nil
DIAMOND DRILL RECORD NAME O F PROPERTY——..,~. ,. ..~ MBL 86-5
Massive Energy Limited
SHEET NO. .FOOTAGE
r ROM
362.2
370.5
371.0
387.4
TO
370.5
371.0
387.8
405. 4
DESCRIPTION
Sheared Greywacke- biotite rich greywacke with biotite alonefoliation at 70" to C/A- becomes more sheared with increasingchloritic alteration toward mineralized area.
Mineralized Greywacke- mineralized section between shearedgreywacke and garnetiferous greywacke- very siliceous with quartz crystals edge:and between tiny fractures- 2% PYRITE- 'H ARGENTITE- some biotite porphyroblasts evident
Siliceous Greywacke- foliation at SO 0 to C/A- very siliceous - fine to medium grained371.0-375.3: garnets up to 1/8" ; 20%
distributed equally through out section
- some shearing evident175.3-175.6: SHEARED PEGMATITE
- continuation of garnets from375.3 ft. to 375.6 ft.376.6-376.7: quartz-carbonate stringer at25 0 to C/A
- foliation at 40" to C/A379.6-381.5: beds of short shearedchloritic sections withquartz ve i ns .
Sheared Siliceous Greywacke- fine to medium grainjd. More shearedthan previous section.387.8-389.3: garnetiferous with chloritic
alteration
SAMPLE
wo
86148614
8614
861.
861
X SUl*M
23
4
5
6
364. 0368.8
372.8
382.0
387.0
FOOTAGE
368.372.
376.
387.0
390.5
i 4. 7i 4.0
7 3.9
5.0
3.5
*KVf ys Ag-. i or row
TrTr
0.03
Tr
T r
bf TON
Nil17. 11
9.77
Nil
Nil
DIAMOND DRILL RECORD NAME OF PROPERTY Massive Energy Limited MOI.E NO MBL 66-5—-—-————— SHEET NO.____;
FOOTAGE
r now
405.4
414.5
TO
414.4
444.5
DESCRIPTION
-mineralization is massive - 15%-and follows foliation at 60 0 toC /A
389.3-392.4: short fine garnet sections atapproximately 1 ft intervals
-some chlorite alteration392.4-393.3: MINERALIZED ZONE
-301 garnets with 1/8" diameter15t pyrite along fractures
402.0-403.3: SMALL MINERALIZED ZONE-5% garnets-21 pyrite stringers parallel tofoliation
403.3-405.4: fine grained garnets
Pegmatite- slightly potassic- contacts at both ends contain more siliceoigreenish quartz for 4".
Silicieous Sheared Greywacke- trace pyrite along foliation414.5-415.4: garnets with pyrite stringers
(31) parallel to foliationat 60" to C /h.
416.3: quartz vein at 70" to C/a416.3-416.8: garnetiferous mineralizedshear zone
- garnet porphyroblasts 1/4"diameter
- 4* pyrite417.6-418.0: chlorite alteration429.8-430.1: mineralized along foliation at
30 0 to C/A- chloritic with 5t PYRITE
437.1-438.0: sheared quartz vein
SAMPLE
NO
1614
3614
s
8614
861! 861!861!861!
•XHM'K
IOC!
'
i
9
0 123
i
fOOTAGErftow
390.5
400.0
414.4
425. 7 430.2434. 1438.0
10
394.8
405. .
418.
430. 2 434. 1438.0443.0
lOML
4.3
5.3
4.0
4.5 3.93. 95.0
AAtfYS Aq
i
1 i
01. TON
Tr
Tr
T r
TrTrTrTr
til TOW
Nil
Nil
i
Nil
NilNilNil
1.41
DIAMOND DRILL RECORD NAME OF PROPERTY Massive Energy Limited^HOI F NO MSL 86-5________________ SHEET NO 9
FOOTAGE
r ROM
444.5
445.1
447. 3
to
445.1
447.3
459.8
DESCRIPTION
438.8-439.5: 31 PYRITE, and garnetsparallel to foliation at 50'C/h
439.9-440.0: quartz vein at 40 0 to C/A440.0-443.1: garnetiferous and sheared
Pegmatite- trace .garnets- biotite inclusions at 10" to C/A
Biotite Greywacke- strong biotite at 40" to C/A and paralic
to foliation- quartz-carbonate stringers along foliat:
plane.
Sheared Siliceous Greywacke- chloritic sections- foliation at 60 0 to C/A
451.0: quartz veins452.0
450.0-450.5: sheared and chloritic450.5-459.0: increasing amount of
biotite shards parallel Lofoliation at 60" to C/A
459.0-459.8: quartz and fine dissemin ated pyrite along foliation
- also along fractures atright angles to foliation
459.8-466.0: trace small garnets463.4-470.0: sections almost completely
silica duo to silica flood ing. Follows remnant bedsparallel to foliation.
- foliation at 60" to C/A.470.0-472.0: increasing biotite along
foliation.
SAMPLE
NO
1
on
861!
861!
861
\ lUl'M
IOCS
4
5
5
FOOTAGErnOM
454.0
458.0
461.0
10 101*1
i
458.0
461 .0
466. 0
4 . 0
3. 0
*ftlT* Ag
1."
l5 . 0 j
i
i
\ 01 ro*
Tr
Tr
Tr
tit T ON
i
1
Nil
Nil
Ni 1
1
DIAMOND DRILL RECORD NAME OF PROPERTY Massive Energy Limited MOLE NO. __MSL 86-5______ SHEET NO 10FOOT AGE
r ROM
459.8
500.0
TO
500.0
DESCRIPTION
Siliceous Greywacke- very siliceous- biotite and sericite parallel to foliatiorat 30" to C/A
488.0: foliation now at 50" toC/A
490.5-490.9: sheared494.6-495.2
496.1-496.2: trace garnets 1/8" diameter496.5-498.6: very siliceous sections as in463.4-470.0 ft.498.6-498.9: quartz-carbonate vein at 60"to C/A and parallel tofoliation.
498.9-500.0: rich in silicaEnd of Hole
l^ti W43-
Peter EitutisMarch 30, 1986
SAMPLE
"0 \ SUL'N,
lOt!F DOT AGt
rnoM TO tOI*i
ASSAYS
-.
'
01 r on bf ton
1
i
'
DIAMOND DRILL RECORDNAME OF PROPERTY Massive Borland Lake________MBL 86-6 , C kl ^ TU 340 feet
-bpc- MJSH MIOT COW-OKA TION INC.
HOLE NO.
LOCATION
LATI TUOE
ELEVATION
LENGTH
Borland Lake GridLO+50E DEPARTURE 1 + 75S
004". AZIMUTH
STARTED March 28. 1986____ DIP
March 29. 1986
FOOTAGE
340
DIP
-37"
AZIMUTH
004"
FOOTAGE DIP AZIMUTHHOLE NO. 66-6 SHEET NO. __i.
REMARKS Casing pulled
LOGGED BY Konnpfh w,FOOTAGE
FROM
0
57.0
67.0
r
TO
57.0
67.0
111.4
DESCRIPTION
Casing in Overburden
Greywacke - fine grained with a slight foliation at irregular angles; strongly dragfolded along core
axis with slight carbonate alteration associated with brecciated sections; trace pyrite along fracturi planes.
Biotitif erous Greywacke - moderate foliation at 50" to C/A with204 biotite phencrysts marking foliation planes;
good silicification evident; trace very fine grained pyrite evident along foliation planes; some sections brecciated with weak carbonatization associated.71.0-72.4: Pegmatite 72.9-73.3: brecciated and dragfolded
section with weak carbonatealteration.
78.3-79.0: broken/ground core. 80.0-86.0: Trace to H pyrite 85.6-86.0
86.7-87.8: 3% pyrite in irregular string ers associated with biotite-rich zone; trace Marcasite.
88.0-89.2: White Pegmatite 89.5-89.791.3-91.6: brecciated greywacke zone with 92.1-92.8 slight carbonate alteration.
SAMPLE
NO.
86H
•MM -
7 34
FOOTAGEFROM
85.0
ro
88. 0
TOTAL
3.0
A fcfi A VA\
v i; OZ/TON
T r
02/TON
Ni J
l
DIAMOND DRILL RECORD NAME OF
MOLE NO.Massive Bo r l and, kak.e.
SHEET NO.___zFOOTAGE
f ROM
111.4
128.3
TO
128.3
142.4
DESCRIPTION
103.4-104.2104.5-105.1: White Pegmatite
108.1109.1-109.6
Siliceous Greywacke- slightly to moderately siliceous andfine grained; slight foliation at 60" to C/A; finegrained biotite shards mark the foliation planes.
112.0: weak stringer of pyritein sheared and siliceoussection.
115.7-116.8: siliceous Pegmatite; near t tselvage.
125.0-127.0: siliceous greywacke becomesmoderately sheared withsiliceous, angular porphy-roblasts evident in a finegrained siliceous matrix.127.8-128.3: sheared and chloritic grey wacke with a strong foliat ion at 60" to C/A.
Garnetiferous Greywacke- sheared and highly bioti tiferous grey wacke with sections exhibiting up to20% garnet porphyroblasts up to 1/4"in diameter; strong foliation at 65" toC/A; up to 54 disseminated pyriteassociated with the garnetiferous sect ions.135.2-136.1: 20% garnet porphyroblasts
with 5% stringer pyrite.137.2-137.4; White Pegmatite.138. 2-139.2
SAMPLE
MO.
861!861!86K
\ SUl'H
ID(S
890
FOOTAGEJ*0"
127.0132.2134. 4
ro
132.2134.4137.0
Torit
5.22.22.6
l
ASSAYSa n irt
x o* TD*
TrTrTr
' ' j ——01 TOM
Nil iNilNil
DIAMOND DRILL RECORD NAME OF PROPERTY,
HOLE NO. __MBL R6-Borland-Lake^
SHEET NO. . -3.TOOT AGE
r BOM
142.4
143.1
153.5
176.2
196.2
*
TO
143.1
153.5
176.2
196.2
208.;
DESCRIPTION
Pegmatite Dyke- white pegmatite with sericitic selvages
Siliceous Greywacke- very siliceous greywacke, massive toslightly foliated and black; grades into opaquelysiliceous section carrying Trace to 14 finelydisseminated pyrite along foliation planes at 144.0148.5-148.8: Pegmatite selvage.150.0-151.0: broken core.
Greywacke- finely bedded to sheared over shortsections; trace pyrite along fracture/foliationplanes.167.7-168.9: Pegmatite171.2-172.2: siliceous/sheared section
with 104 pyrite inirregular stringers.
Mineralized Greywacke- highly sheared and silicified zone withsheared and chloritic contact zone at 176 feet;strong foliation at 30 0 to C /h especially in biotite-rich sections; good sulfide mineraJ ization through out in disseminations and irregular stringers; 101total sulfide throughout core length: 54 stringerpyrite, 34 argcnti te/galcna , 2?, sphalerite inirregular masses.
185.0-186.0: 34 sphalerite187.0-188.0: up to 54 argent i tc-galena
mixture.
Potassic Pegmatite Dyke- megacrystic with trace pyrite alongfractures.
SAMPLE
NO.
86168616
86K861f86K86K86K86K8611861861861
l SULPM iOCS
12
34567890'l2
FOOT ACEf*OM
141.0143.0
171.5172.5176.0182.0187.0192. 3196.3208.0212.0217.0
TO
143.148.
172.5176.0182.0187.0192.3196. 3208.0212.0217. 0220.0
TOT4L
) 2.01 5.0
1.03. 56.05.05.34.0
11.74.05. 03.0
ASSAYSAn An
*. 01 TO*
TrTr
TrTr
0.010.010.030.03TrTr
0. 050.06
——— -J ———
01 TOM
NilNil
NilNil18.4319. 35j26. 2910.95NilNi 19. 6i
21 . 1C
11.4
J
/4/i
DIAMOND DRILL RECORD NAME OF PROPERTY Massive Bor]and,Lake, MBL 86-6
.————^-———-——.-.___.... '.MEET H O. ^__MOLE NO. .
root ACEf MOM
208.0
234.6
243. 3
306.5
TO
234.6
243. 3
306. 5
340.0
DESCRIPTION
Greywacke- finely bedded greywacke with a moderatefoliation at 60" to C/A; some sheared sectionsexhibit chloritic and carbonate alteration.214.3-218.1: sheared and siliceous
section with 2% disseminatetpyrite; 11 argentite/galena
236.0: Pegmatite.
Siliceous Greywacke- as previous; clots of disseminatedsericite throughout.
Biotitif erous Greywacke- strong foliation with 101 to 15% biotitishards marking foliation planes; strong foliationat 25" to C/A.248.8-249.8: contact zone with pegmatite
dyke; 10% pyrite withoccasional garnet porphy roblast.
249.8-251.7: Potassic Pegmatite Dyke258.0-260.6: sheared and carbonaceoussection with 2 1 pyrite instringers .
270. 7-272. 7274. 0-276.7277.3-278.7: White Pegmatite Dyke.279. 1-279. 8282.0-282.9
287.0: stringer of argentite 1/8inch in width.
- at 290.0 feet foliation is at 35 0 to C/Siliceous Greywacke
- as previous with slight foliation at
SAMPLE
NO.
8611861'
861"
861'
^-
1 lUl*"
IO(S
34
5
6
FOOTACtf *OM
247.0251.7
257.0
286. 0
10
251.7253.7
262.0
288.0
'01*1
4. 72.0
5.0
2.0
ASSAYSAn An
l 01 TO*
0.07Tr
Tr
Tr
b t TO*
23.38Nil l
Nil
Ni l
DIAMOND DRILL RECORD NAME OF PROPER TV Massive Borland LakeHOLE NO. . MBL 86-6 _ ^ SHEET
TOOT AGE
r MOM TO
340.0
DESCRIPTION
40" to C/A.312.5-313.0: chloritic shear zone317.3-317.6: siliceous shear zone. 319.1: quartz-carbonate vein at 50" to C/A; 20% pyrite associatec
width 1/4 inch.321.4: fracture at 50" to C/A with
trace argentite.326.2-327.2: sheared and garnetiferoussection with banding at 60"to C/A; hematite alongfractures parallel tofoliation; vuggy quartzcarbonate stringer evident;trace argentite.331.2-332.0: quartz-carbonate vein withsericitic alteration alongselvages.
- bedding at 45" to C/A evident.
End of Hole
Kenneth W/ JohnsonMarch 29, 1986
SAMf'LC
..0
8617 8617
\ lUL^H
iocs
7 8
f DOT *CCr •O 4'
318.0 323.0
'o
323.1 328.
IOt'1
) 5.0 3 5.0
ASWS Ag-. i oi - ron
0.03 Tr
b l T DK
0. 87 Nil
;r1
FELSIC INTRUSIVE ROCKS
Pi Pink PegmatiteP; While PegmatiteAi ApliteGc Sheared Granite, Feldspar Augen Gneiss
Si Granite
MAFIC AND ULTRA MAFIC INTRUSIVE ROCKS
60 Diorite 6b Gabbro
6c Peridotite
CHEMICAL METASEDIMENTS
5a Chert
5b Limestone5c Oxide Facies Iron Formation5d Sulphide Facies Iron Formation
l 4 j CLASTIC METASEDIMENTS
4a Quartzite
4b Siliceous Metagreywacke4c Metagreywocke
4d Argilite
4e Sericitic Metagreywocke
4f Sillimanite Schist
4g Tuffaceous Sediments
FELSIC VOLCANICS
3o Flows
3b Tuffs
3c Lapilli Tuff3d Agglomerate3e Cherty Tuff
INTERMEDIATE VOLCANICS
2o Flows
2 b Tuffs2c Lapilli Tuff2d AgglomeroTic Tuff
MAFIC VOLCANICS
lo Undifferentioled Flows
Ib Medium Groined Flowsle Pillowed Flows
Id Amphibolitized Volcanic
le Tuff
SYMBOLS
Area Of Bedrock Outcrop
Bedding, Strike And Dip
Foliation, Strike And Dip
Joint Ptone
Fault With Displacement
Shear Zone
TIE LINE 15 N
5N
BASE LINE 00
5 S
10 S
Borland L oke
LEGEND
SHEET LAYOUT
WEST
l
EAST
BUSH PILOT CORPORATION
Massive Energy/Noranda Option BORLAND L AKE PROJECT, ONTARIO
PLAN OF DIAMOND DRILLINGWEST SHEET
SCALE 1":100 FEET APRIL 1986
ANADA
Dwg. No E.'C.
53D16NEa084 63.4856 BORLAND LAKE S00
B o r l a n d L oke
BASE LINE 00097 D )
10 S
BUSH PILOT CORPORATION
Massive Energy/Noranda Option BORLAND LAKE PROJECT. ONTARIO
PLAN OF DIAMOND DRILLINGEAST SHEET
SCALE 1":100 FEET APRIL 1986
TDRQNTO CANADA
Dwg. No E.I.C
Q/fl
53D16NEM84 63.4856 BORLAND LAKE 210
3s d
TIM
IM3M
7 M
—
.4—-
1 to
S3D16NE0004
63.4856
BORLAND
LAKE
r
i ^n an
*ii.
.
O1
IMIM
-—-..
.,3
!IM
UV7SC - i
L2
if. IM
OO
1 to
\
p
53D16Nee004
63.4856
BORLAND
LAKE
230
v- -
---"*
- ni
r if-
*- f
*'
IM•j
,*^
ai.
iii.
^- i
t-^
i
3'IM
ara
SIM
e1 M
\
L2
36-'V
2-
+Z5E
x
3*^0
53
0 oo
-V-
At.
o-o
h O
'.A
"X.
53D
16N
E00
04
63
.48
56
B
OR
LAN
D
LAK
E2
40
•l—
*li
-W-J
—
*-.
'
1 to
.***^n
riQ
ST
?
-
J...^
&JF-
"' : ;r
l
I'M
IMai
\iS4
\l
1 to
53D
16N
E0I
B04
6
3.4
85
6
BO
RLA
ND
L
AK
E2
50
V
260
*-
Jjt:
roUJ UJ
roUJ10
UJ LUr-
UJ CO
UJen
SL Lake Level
100 L
200L
300 L
400 L
65-27V?
65-1995
•i
BLOCK 'A
53016NEOei84 63.4856 BORLAND LAKE
270
In com p l e t e
Drilling
29V
Water
Lacustrine Clay
23
Incomplete
Drilling
65-9
BLOCK 'C
MASSIVE ENERGY LTD.BORLAND LAKE PROPERTY - ONTARIO
VERTICAL LONGITUDINAL SECTION
BLOCK 'B 1
A GGRADE-THICKNESS CONTOURS
40 8O l 2O 160
FE ET
D. A. Bourne, K.W.Johnson April , 1986
O
IOOL
200L
300 L
400 L
500 L
ro
o"
3,875 8- 66, 0-03
65-27
53DI6NE0004 63.4856 BORLAND LAKE
O6S-/9
4,1676'66,0-03
o 8
3,0839-44 t O-OI
BLOCK 'A 1
Incomplete
Drilling
X-RAY 2O
10,91711-83,0-03
29
85-3
23,2921310, O 03
85-1
X-RAYI O
29,0838-96,0 03
65-18
65-4
85-2
46,10012 93,0-02
65-2
LU
69,1677 87, O 01
^ 9
65-l
28
LU OJ
55-3
28,875911 , TR
65-14
15
20,1259-91,0 01
23,0416-01 , TR
86-5
O86-4
Lacustrine Clay
LJ m
LJ iuin
LU(D
LJN
LU GO
Lake LevelWater
O10
65-tl
22,8753-92,0 O
27
65-15
36,6666 74, TR
37,2327-07, 0-01
26
O86-1
86-3
BLOCK 'B 1
55-5O
20,27111-28,0 04
55-5
14 O
6,937619,O 08
65-7
8,6045-60,0-07
86-2O
Incomplete
Dri M ing
LEGEND
8 O-
2,083-9-44,0-01
-MINERAL INVENTORY BLOCK
D.D. HOLE NUMBER
PIERCE POINT OF D.D.HOLE
-TONS
-oz Ag , oz Au
65-16 O
2,0833 52 .0-01
5,4165-50,0-02
23
25,0004 66, 0-O3
55-5
17
6,1587-92,0 12
25
65-9
BLOCK 'C 1
MASSIVE ENERGY LTD.BORLAND LAKE PROPERTY - ONTARIO
VERTICAL LONGITUDINAL SECTION GEOLOGICAL MINERAL INVENTORY
400 l
800 200 i
1600
FE ET
D A. Bourne, K.W.Johnson April , 1986
u en
\
63.4856 BORLAND LAKE 230
LEGEND
Interpreted fault showing basis for projection .. . ..
M - Magnetics V - VLF EM (NAA)
Projected geologic contact
AEM conductor axis... ...
Ultramafic intrusion or plug
BUSH PILOT CORPORATION
Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO
ELEMENTS OF STRUCTURE
SCALE 1:10,000 MAY 1986
EXCAL1BUR INTERNATIONAL CONSULTAMTS LTD.
TORONTO, CANADA
Dwg, No. E.I.C.- 1678
in rO rO
rOro
oo rO rO
OrO
5SOJ
CO OJ
?(M OJ
in OJ OJ
rO OJ
OvJ
OJ OJoOJ 00 ro Osi O
t C', , 4500NTIE LINE 15 N
10 N
BASE LINE 00
5 S
10 S
B or l a nd
ic'2 ,3700SL oke
SHEET LAYOUT
EAST
LEGEND
Instrument: Rx-Huntec Mk IV, Tx-Phoenix 1PT-1 Electrode configuration: Gradient array, 0 = 100' Chargeability contour interval....... 5 msecs25msec contour. 5 msec contour. De press ion.......
BUSH PILOT CORPORATION
Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO
CHARGEABILITY CONTOURS Gradient Array
WEST SHEETSCALE 1^100 FEET APRIL 1986
Dwg. No. E.I.C-I679A53DI6NE0B04 63.4856 BORLAND LAKE
300
t C,,4300N
BASE LINE 00(Bearing 097 0 }
B o r and L okeT C 2 ,4200S
BUSH PILOT CORPORATION
Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO
Instrument: Rx-Huntec Mk!V, Tx-Phoenix IPT-1 Electrode configuration: Gradientarray.a =IOO Chargeability contour interval....... 5 m sees25msec contour 5msec contour. Depression
SHEET LAYOUT
CHARGEABILITY CONTOURS Gradient Array
EAST SHEETSCALE 1=100 FEET APRIL 1986
Dwq. No. E.I.C-I679B53D16NEC0&4 63.4856 BORLAND LAKE
m ro ro
ro rO
CO PO
OrO
O CO
CO CO
h- oo
toCNJ
toC\J (\J
roCO
CM CO CO
oCJ
tCO r- rO OJ O
Ci, 4500NTIE LINE 15 N
BASE LINE 00
5 S
10 S
B o r l Q n d
|C'2 ,3700SL oke
SHEET LAYOUT
WEST EAST
LEGEND
Instrument: RxHuntecMk IV ,Tx- Phoenix l PT-1 Electrode configuration: Gradient array,a z IOO' Contours of apparent resistivity int. lOOOflm 5000am contour. 1000 firn contour. Depression ........,....100 a 200Urn contours within anomalously low domain.
BUSH PILOT CORPORATION
Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO
RESISTIVITY CONTOURS Gradient Array
WEST SHEETSCALE 1"-100 FEET APRIL 1986
Dwg. No. E.I.C.-1680A53D16NE00IB4 63.4856 B ORLAND LAKE 320
4 C,,4300N
TIE LINE ION
BASE LINE 00
B o r land L okeC 2 ,4200S
BUSH PILOT CORPORATION
Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO
Instrument; Rx-Huntec MklV, Tx-Pnoemx l PT-1 Electrode configurofion: Gradient array, a = Contours of apparent resistivity int.lOOOOm 5000 Jim contour 1000 Dm contour Depression .100 8r 200 H m contours within anomalously low domain
SHEET LAYOUTRESISTIVITY CONTOURS
Gradient ArrayEAST SHEET
SCALE 1=100 FEET APRIL 1986
Dwg. No. E.I.C.-I680B53D16NE6004 63.4856 BORLAND LAKE
LOro PO
rO PO
00rO rO
OrO
(T) 00
CO 00
r-CO
o?00
lO 00 00
ro 00
0000
o00 a.) r- U") •r rO CO
TIE LINE 15 N
5 N
BASE LINE 00
10 S J lil O
B or l on d L oke
SHEET LAYOUT
WEST EAST
LEGEND Instrument....... ........Gem Systems GSM-8Bose station.................,......CMG MR-10Total field base level.............. 59,000 nTContour interval........................... 50nT5000 nT contour.500nT contour.50 nT contourDepression.............................r"*
BUSH PILOT CORPORATION
Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO
TOTAL FIELD MAGNETIC CONTOURS
WEST SHEETSCALE 1"^100 FEET APRIL 1986
53D16NE8004 63.4856 BORLAND LAKE 3-40 Dwg. No. E.I.CH68IA
00 (D ro c\JO O
UJ OJ
UJ
roUJ UJ
inUJ
(D
LJr-
UJ
CO
LJ
(D
UJ
OUJ UJ
CMUJ rO
UJ
inUJ UJ UJ
COUJ CD
UJ
oCM
B o r l an d L oke
SHEET LAYOUT
WEST EAST
LEGEND Instrument ................Gem Systems GSM-8Base station.......................CMG MR-10Total field base leveL............. 59,000 nTContour interval........................ 50 nT5000 nT contour,. 500 nT contour. 50nT contour Depression
BUSH PILOT CORPORATION
TIE LINE ION
5 N
BASE LINE 00
10 S
Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO
TOTAL FIELD MAGNETIC CONTOURS
EAST SHEETSCALE 1"^ 100 FEET r APRIL 1986
53DI6NE0004 63.4656 BORLAND LAKE Dwg. No EIC.-I68IB3S0Q/7?
Zoneapprox. position only )
S o l o n Pon
BASE LINE 00
LTRAMAFIC
AFIC INTRUSION
f a n d L oke
BUSH PILOT CORPORATIONLEGEND
Mineral prospect, horizon......
Polarization axis of note .....
Polarization ring structure
Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO
Interpreted fault showing relative movement and basis for projection
M — MagneticsV - VLF EM (NAA)G — GeologyD — Drilling
SHEET LAYOUT
INTERPRETATIONWEST SHEET
Iron formation marker horizon
SCALE 1"MOO FEETProposed DDH with identification and horizontal projection
Geologic contact inferred ..
Postulated fold axis synclinal , anticlinal.
Dwg.No.E.I.C.I682A53D16NE0004 63.4856 BORLAWD LAKE
N0.86-G3
ETA VOLCANO -SEDIMENTARY DOMAIN
ULTRAMAFIC NTRUSION
So r land L oke
BUSH PILOT CORPORATIONLEGEND
Mineral prospect, horizon
Polarization axis of note .....^—
Polarization ring structure**"
Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIOInterpreted fault showing
relative movement and basis for projection
M - MagneticsV - VLF EM (NAA)G — GeologyD - Drilling
INTERPRETATIONEAST SHEETIron formation marker
horizor SCALE 1-100 FEETProposed DDH with ldent,fication and . horizontal projector
n —— -- No 86-G2Geologic contact inferred.... ——
Postulated fold axis synclinal, anticlinal
.r — — r —
Dwg.No. E.I.C I682B
370