New Orientation Model
Confirmed.
Potential to Greatly Expand Morley
Opens
VANCOUVER, BC, Dec 8, 2020 /CNW/ - Tajiri Resources
Corp. (the "Company") (TSXV: TAJ) is delighted to
report initial results from first pass RC drilling at the
Morley Prospect situated within the Company's 1,162km2
Reo Gold Project, located at the confluence of the prolific Hounde,
Boromo and Goren Greenstone Belts, Burkina Faso (Figure 1). The shallow, 23
hole program intercepted consistent gold mineralization
including:
![Figures 1 through 6 (CNW Group/Tajiri Resources Corp.) Figures 1 through 6 (CNW Group/Tajiri Resources Corp.)](https://mma.prnewswire.com/media/1361065/Tajiri_Resources_Corp__Tajiri_Drills_11m___8_6g_t_Au_including_3.pdf?p=pdfthumbnail)
•
|
3m @ 30.9g/t
from 24m;
|
within 11m @
8.6g/t from 20m;
|
MTRC0022
|
•
|
1m @ 18.0 g/t
from 17m;
|
within 13m @
1.9g/t from 15m;
|
MTRC004
|
•
|
1m @ 17.0g/t
from 51m;
|
|
MTRC0015
|
•
|
2m @ 11.8g/t
from 31m;
|
|
MTRC0011
|
•
|
2m @ 11.3g/t
from 32m;
|
within 17m @
1.6g/t from 18m;
|
MTRC0014
|
•
|
1m @ 4.3g/t
from 41m;
|
within 5m @ 1.7g/t
from 39m
|
MTRC0014
|
•
|
1m @ 10.8g/t
from 75m;
|
within 6m @ 2.7g/t
from 75m;
|
MTRC005
|
•
|
2m
@ 7.5g/t from 34m;
|
within 7m @ 2.7g/t
from 30m;
|
MTRC005
|
•
|
1m
@ 8.9g/t from 64m;
|
within 10m @ 1.2g/t
from 60m;
|
MTRC0020
|
•
|
2m
@ 4.6g/t from 55m;
|
within 8m @
1.3g/t from 51m;
|
MTRC006
|
•
|
2m
@ 4.8g/t from 59m;
|
within19m @ 1.3g/t
from 59m;
|
MTRC009
|
•
|
1m
@ 4.2g/t from 82m;
|
|
MTRC007
|
Results of all drill holes are given in the Table at the end of
this document and shown in Figure 2.
The results reported today are the product of a drill program
designed as a first test of Tajiri's new model for the orientation
of mineralisation at Morley. These results, when combined
with historic drill intersections, largely confirm the new model
and opens new and hitherto sparsely to completely unexplored strike
and dip directions to expand Morley. Historic results include:
•
|
8m @ 54.2g/t
from 16m;
|
within 32m @
17.4g/t from 4m;
|
KRAC128
|
•
|
4m @ 57.8g/t
from 8m;
|
within 16m @
14.8g/t from 2m;
|
KRAB008
|
•
|
4m @ 15.6g/t
from 78m;
|
within 14m
@ 6.9g/t from 70m;
|
MRRC005
|
•
|
1m @ 75.5g/t
from 33m;
|
within 18m
@ 5.5 g/t from 33m;
|
MRRC040
|
•
|
2m @ 15.1g/t
from 24m; &
|
|
|
|
1m @ 11.6g/t
from 47m; &
|
|
|
|
2m
@ 5.3g/t from 18m; &
|
|
|
|
1m
@ 5.1g/t from 33m; &
|
|
|
|
1m
@ 5.8g/t from 44m
|
within 40m @
2.6g/t from 8m;
|
KRAC011
|
•
|
8m @ 9.3g/t
from 16m; &
|
|
|
|
2m @ 8.3g/t
from 8m;
|
within 30m @
2.7g/t from 8m;
|
KRC022
|
•
|
2m @ 15.6g/t
from 42m; &
|
|
|
|
2m@ 7.1g/t
from 14m; &
|
|
|
|
2m @7.0g/t
from 24m; &
|
|
|
|
2m @ 4.9g/t
from 36m;
|
within 42m @ 2.1g/t
from 8m;
|
KRC020
|
•
|
1m @ 32.5g/t
from 17m;
|
within 25m @
1.9g/t from 14m;
|
MRRC001
|
•
|
2m@ 11.1g/t
from 0m;
|
within 11m @
2.9g/t from 0m;
|
KDH003
|
•
|
1m @ 21.9g/t
from 36m;
|
within 21m @
1.8g/t from 29m;
|
MRRC002
|
•
|
2m @ 10.3g/t
from 58m;
|
within 8m @
2.8g/t from 58m;
|
KRC0441
|
________________________________
|
1
|
All historic
intercepts are from drilling at a variety of azimuths and dips to
mineralisation and individual intersections may not be
representative of true widths and may vary ~ 20 to 80% from true
width. New results are interpreted as being within 80-90% of true
widths.
|
Summary
- Tajiri's maiden drill program, importantly, confirms a new
orientation model for gold mineralisation at Morley which is situated in a belt scale
deformed granite and lies within 800m
of the northern and 1,000m of the
western granite-greenstone contact (Figure 1).
- Exploration at Morley is still
at an early stage- historically it has returned high grades from
drill holes over widths that make it a high priority target but a
coherent model of the orientations and structural controls of
mineralisation was never previously established.
- Our drilling shows the main mineralised zone at Morley has a WNW strike and dips -50˚
northeast. Strike is subparallel to a set of crosscutting
shear zones which occur over a width of about 2km at Morley and are axial to a major 40˚ flexure in
the strike of the granite-greenstone belt from ENE to NNE (Figure
6).
- Most Importantly confirmation of the new model opens-up on
strike and down dip potential into very sparsely explored or
totally unexplored areas both immediately and further along strike
(Figures 4,5 & 6).
- A very favourable target is now in play: only
1,000m WNW along strike, the
"Morley structure" cross cuts the
ENE trending sheared granite-greenstone contact of the Morley host granite. Empirically,
granite-greenstone contacts are a favoured location for high grade
gold deposits in Burkina such as M1 South, Siou and Yaramoko
(Figure 6).
- This target area is under alluvial cover and has never been
sampled and represents a first order opportunity for Tajiri.
- At Morley mineralisation
presents as high-grade narrower veins within broader halos of
low-grade sericite + carbonate +/- pyrite shearing. It is
expected that veins may have an orientation oblique to shearing and
there may be at least two sets (Figure 3).
- While drilling has broadly confirmed the strike and dip of the
model it requires further work on the details to explain grade and
thickness variations within the mineralised zones. This is
likely the influence of a second structural direction on vein set
orientation within the shear zones and/or the presence of
intersections with other structures of different orientations.
- Several lines of evidence point to the second structural
control being either NNE or ENE with a likely 50˚-60˚ north
dip. Strike of the second structural control is therefore
subparallel to the major belt scale shear zones in the area.
- Balance of evidence suggests the high-grade intersections
returned in KRAC128 (8m @
54.2g/t) and MTRC 022 (3m @
30.9g/t), which we drilled as a scissor hole, are from a NNE
striking vein which dips 50˚ to 60˚ to the west or it is the
intersection of ENE and NNE vein sets with ~50˚ degree dips to the
west. ENE strike projections of this vein have been
adequately tested by historic drilling but not NNE directions as
most N-S oriented RC drillholes are subparallel to this
direction. Significantly this vein in RC chips appears to
have a different character to those of other vein zones drilled
during the program appearing to be more of a laminated style.
- Historic close spaced (50m x
50m) auger drilling to sample top of
saprolite in the immediate vicinity of the Prospect confirmed WNW,
as well as NNE and ENE trends as anomalous and the close spaced
auger anomaly remains open in all of those directions (Figure
4).
- Historic scout drilling oriented on NW-SE lines, intersected
thin or low-grade mineralisation on ENE and possibly NNE trends
(Figure 4).
- There is a good potential for Morley to be a stacked lode
system with gross strike controlled by ENE or NNE bounding
shears and main lodes in crosscutting WNW strike and NE dip
orientations. This possibility remains poorly tested
but could lead to Morley becoming
a substantial stand-alone deposit (Figure 5).
- Prospect has excellent opportunities to host high grade
intersection shoots, but suspected plunge directions and best
intersection structures still need to be determined.
- Demonstrating that WNW structures are mineralised has important
implications for exploration elsewhere within the Reo Project as
historic sampling patterns are orthogonal to the NE trending main
belt structures and thus poorly oriented to test potentially WNW
mineralised structures.
- Given the above potential two structural controls, drilling has
been paused temporarily to gather more structural data to optimise
drill directions. To this end the company will embark on a
focussed deep trenching program to gather structural data and vein
orientation data before re-commencing drilling at the prospect
scale. Trenching will commence early Q1 2021 after a
contracted excavator finishes work at the K4-K5 Prospect, 20km to
the south.
- Close space power auger drilling is being planned to step out
along potential strike directions in the immediate vicinity of
Morley prior to further work.
- RAB/ Aircore rig options being investigated to test granite
greenstone contact target WNW of Morley.
Chairman's Comment
Executive Chairman, Dominic
O'Sullivan remarked:
"I am simply thrilled that with the Company's first modest
expenditure in Burkina of about USD200,000, we have not only returned some great
results but have also established several fairways along which
Morley might grow from a modest
sized prospect into a potentially much larger one.
We are developing our understanding of the deposit, starting
from a rather higgledy piggledy set of drilling with holes and
grades going in all directions, into a geologically cogent
framework that demonstrates potential for a lot more at
Morley. It fits our philosophy - find a poorly
understood or overlooked discovery, in a Tier one address and do
the hard yakka, looking at all the data from every angle, then
follow-up with smart prudent focused exploration.
I'm particularly enthused about the on-strike potential
generated by confirming that WNW oriented structures at
Morley host gold mineralisation,
especially just west of Morley,
where the "Morley Structure," smashes an 800m sinistral displacement into a sheared
granite-greenstone contact which itself has a dextral reverse sense
of movement. This creates a WNW trending
granite-greenstone contact, hugged by the Morley structure for about 800m of strike. That spells a lot of
dilation on favourable structures and lithological contrasts.
What's not to like about that? As it's under cover, never
seen before, I feel it's a bit like a little Chrissy prezzie for
us- still under the tree, all wrapped up and we can't wait to
open it."
Details of the Morley Drill Program
Results reported today are Tajiri's first steps in our
exploration at Morley and as a
necessary first precedent to further work it has focused on
defining the orientation of mineralisation.
Historically, the orientation of mineralisation has
been poorly constrained, and several equivocal interpretations
could fit historic data due to the following:
- Drilling was conducted blind because of a thin veneer
(3-10m thick) of cover overlying the
Prospect;
- Morley is hosted by a single
relatively undifferentiated granite lithology and a lack of other
lithologies meant models could only be constructed by grade
interpolation;
- Morley lies in a zone of
considerable structural complexity, near the focus of a change in
the gross strike of the granite-greenstone belt of 40˚ from ENE to
NNE, and major and lessor shears of both orientations together with
numerous WNW, NNW, EW and minor N-S orientations transect the area
(see Figure 6);
- all structures or their intersections could be potential
fairways for mineralisation and all structural orientations can be
associated with some form of gold anomalism, though the ENE- NNE
orientations appear to dominate the distribution of gold anomalism
on a regional scale;
- drilling to date has been suboptimal to test all possible
mineralised orientations and drilling has mostly been oriented
either:
-
- North-south and predominantly drilled to the south or
- On NW-SE oriented scout drill lines of 200-400m spacing with alternate lines drilled to
either the SE or NW.
In our new model, gold mineralisation which occurs as sheeted
high grade quartz veins, within low grade sericite + carbonate +/-
pyrite altered shear zones hosted by a syntectonic belt scale
granitoid is comprised of several 1-20m thick, NW-WNW striking lodes which dip
between 40˚and 55˚ to the NE. The best historically drilled
lode, "the Main Lode" where current drilling has focused, has a
known strike length of about 300m.
Results announced today are highly supportive of our new model
and intersections mostly occur where the model predicted.
Drill results returned to date demonstrate good apparent down-dip
coherence with our model and continuity of between 100m and 150m
(100m vertically below surface- base
of current drilled depth). Zones remain open down dip.
On the other-hand strike direction has only been broadly confirmed
but it is beginning to resolve into a WNW rather than NW
strike. Further work is required because:
- Access to drill the central part of the main lode was
restricted as it is the site of a small forest (Figure 2) and
permission was not granted by the local community to drill within
its confines. Investigation of mineralisation in this area will
require deeper drilling, later, as it is beyond the capability of
the contracted RC rig.
- Mineralisation is abruptly interrupted on the section line
comprised of holes MTRC007, 008, 18 and 009. Hole
MTRC009 intersected a vein zone grading 2m @ 4.8g/t within 19m @ 1.3g/t from 59m and on-strike from mineralisation intersected
in hole MTRC006 to the south (2m @
4.6g/t from 55m; within
8m @ 1.3g/t from 51m) but only weak anomalism was intersected up
dip by MTRC0018 and MTRC008. Based on a feature visible in ground
magnetics, it is possible that a post mineralisation fault striking
NNW, displaces the Main lode with an with apparent dextral throw of
50m. This interpretation fits
with a WNW strike.
- As this was a first pass program and the exact strike of
mineralisation was unknown at the time of planning- being modelled
as between WNW to NW, several holes appear to have collared in the
footwall of the Main lode and did not intersect the expected Main
lode near surface. These holes are MTRC003, 7, 10, 13 and 19
and the lack of mineralisation in those holes up dip from
mineralisation strongly suggest that strike is closer to WNW than
to NW (Figure 2).
Variation in the grades and thickness intersected also suggest
that there is a second structural orientation that influences the
mineralisation at Morley. This second structural
control may be an upshot of vein sets having an orientation which
is oblique to the orientation of the host shear zone, a common
feature of this style of mineralisation but we also believe, based
on the overall architecture of all data, that mineralisation is
developed preferentially within the WNW structures at their
intersection with either ENE or NNE structures that are also
evident in ground magnetic images. Evidence for a second
significant structural control is:
- At the known north end of Morley main lode, it thickens and high-grade
vein densities increase (Figure 3) where it is inferred to be
intersected by an ENE trending shear zone of weaker mineralisation
that was drilled over 400m of strike
going west and which returned a peak value of 14m @ 1.1g/ (Figure 4).
- All three structural orientations align with the overall shape
of a gold in saprolite geochemical anomaly that overlies the
Prospect (Figure 4), suggesting all three alignments may be
mineralised. With lobes and high values extending along WNW,
ENE and NNE orientations. This data was derived from a
Newmont 2008, 50m x 50m auger program down to 10 m depth that covered an area of 1,000 x
850m and was conducted after air-core
scout drilling had located the prospect.
- All three structural orientations align with anomalous gold
values returned by regional reconnaissance saprolite sampling auger
data which was conducted on lines spaced 400-800m apart and samples collected every
100m (Figure 6).
- Several fine scale structures visible in ground magnetics
especially 1VD, 2VD and tilt filtered images coincide with all
three orientations and higher grades in drilling can be tentatively
associated with the intersection of the WNW striking lodes with
both ENE and NNE trending structures.
The above brings the possibility of repeats of WNW oriented
mineralisation along ENE or NNE directions in effect forming a
large-stacked lode system. The orientation of Historic scout
drilling outside of the main area of drilling at Morley has poorly tested this concept with
scout drill lines oriented subparallel to the WNW strike of
mineralisation and lines alternating between down dip and across
dip directions. Better oriented north south holes are
confined to the norther margins of the prospect. Potential is
illustrated in Figure 5
Next steps at Morley
Given the evidence for a second structural control on
mineralisation, we have temporarily paused our drill program to
undertake deep trenching and pitting to gather structural data and
map dominant vein orientations within the shear zones. Once
this is done drill direction/s which is currently on NE-SW lines
drilling to SW can be optimised to intersect vein sets within the
shear zones to give representative grades and investigate
potentially higher-grade plunging intersection shoots.
It is expected that trenching will commence early Q1 2021 after
a contract excavator completes its work at K4-K5.
Close spaced auger power auger drilling is being planned
to extend the Morley footprint in
favourable directions.
Finally, options to contract a RAB/Aircore rig to drill the
covered granite greenstone contact in the area where the "Morley
Structure" intersects it, are being investigated.
Other Exploration
In Burkina
We have commenced trenching at K4-K5 to investigate areas where
cover is thinner – in artisanal workings or where drilling shows
mineralisation close to surface. Purpose of the program
is to collect structural and lithological data and examine
mineralisation near surface as previous drilling has been wide
spaced and we are not sure if dominant trends are NNE or NE
striking. This 2,000m program
is expected to be completed by very early next year after which RC
drilling will be commenced.
We are also in the advanced stages of planning closer spaced
deep auger drilling at K4-K5 to define drill targets within the
larger area of K4-K5 outside planned drill areas. The geochemical
anomaly at K4-K5 is huge and extends over 7 x 6 km.
Part of that program will cover extensions of drilling by Arrow
Minerals (ASX:AMD) announced early this year which shows the
eastern contact of the regional granite which hosts Morley is prospective. This
program is expected to commence shortly.
In Guyana
We have recently completed a small auger program at Epeius to
investigate the strike extensions of good results produced by Troy
Resources (ASX:TRY) just across the projects southern
boundary. Troy's results include drill intersections of
10m @ 6g/t Au, 17m @2.2g/t Au and trench intersections of
13m @ 2.3g/t Au, 8m @ 2.3g/t Au & 11m @ 1.47g/t Au. An announcement will be
made shortly and a follow-up trench program is already underway
with 600m linear metres excavated to
date.
Qualified Person
The Qualified Person under National Instrument 43-101 -
Standards of Disclosure for Mineral Projects for this news
release is Dominic O'Sullivan a
geologist, member of the AusIMM, Executive Chairman of Tajiri
and who has reviewed and approved its contents.
On Behalf of the Board,
Tajiri Resources Corp.
Graham Keevil,
President & CEO
About Tajiri
Tajiri Resources Corp. is a junior gold exploration and
development Company with exploration assets located in two of the
worlds least explored and highly prospective greenstone belts of
Burkina Faso, West Africa and Guyana, South
America. Lead by a team of industry professionals with a
combined 100 plus years experience the Company continues to
generate shareholder value through exploration.
This news release may contain forward-looking statements
based on assumptions and judgments of management regarding future
events or results. Such statements are subject to a variety of
risks and uncertainties which could cause actual events or results
to differ materially from those reflected in the forward-looking
statements. The Company disclaims any intention or obligation to
revise or update such statements.
Neither the TSX
Venture Exchange nor its Regulation Services Provider (as that term
is defined in the policies of the TSX Venture Exchange) accepts
responsibility for the adequacy or accuracy of this
release.
Table of Significant Drill Intersections
|
Hole_Number
|
Dip
|
Azimuth
|
Total
Depth
|
From
|
To
|
Interval
|
Au_ppm
|
|
|
NB: MTRC001 and
MTRC002 were abandoned before reaching target depth and
were redrilled approx.. 10m away from
each collar as MTRC005 & 6
|
|
|
MTRC0001
|
-60
|
225
|
69
|
0
|
1
|
1
|
0.3
|
|
|
|
|
|
|
20
|
30
|
10
|
1.7
|
|
|
Including.
|
|
|
|
28
|
29
|
1
|
3.0
|
|
|
|
|
|
|
42
|
43
|
1
|
0.4
|
|
|
|
|
|
|
49
|
50
|
1
|
0.3
|
|
|
|
|
|
|
59
|
60
|
1
|
0.2
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0002
|
-60
|
225
|
72
|
6
|
8
|
2
|
0.9
|
|
|
|
|
|
|
14
|
15
|
1
|
0.5
|
|
|
|
|
|
|
29
|
30
|
1
|
0.2
|
|
|
|
|
|
|
33
|
35
|
2
|
0.5
|
|
|
|
|
|
|
38
|
39
|
1
|
0.7
|
|
|
|
|
|
|
44
|
48
|
4
|
0.5
|
|
|
Including
|
|
|
|
47
|
48
|
1
|
1.4
|
|
|
|
|
|
|
58
|
62
|
4
|
0.4
|
|
|
Including
|
|
|
|
61
|
62
|
1
|
1.1
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0003
|
-60
|
225
|
81
|
0
|
1
|
1
|
0.3
|
|
|
|
|
|
|
12
|
13
|
1
|
0.2
|
|
|
|
|
|
|
20
|
21
|
1
|
0.3
|
|
|
|
|
|
|
48
|
49
|
1
|
0.3
|
|
|
|
|
|
|
71
|
72
|
1
|
0.4
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0004
|
-60
|
225
|
87
|
3
|
4
|
1
|
0.3
|
|
|
|
|
|
|
15
|
28
|
13
|
1.9
|
|
|
Including
|
|
|
|
17
|
18
|
1
|
18.0
|
|
|
|
|
|
|
77
|
78
|
1
|
0.2
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0005
|
-58
|
225
|
108
|
30
|
37
|
7
|
2.7
|
|
|
Including
|
|
|
|
33
|
36
|
3
|
5.5
|
|
|
|
|
|
|
40
|
41
|
1
|
0.2
|
|
|
|
|
|
|
43
|
44
|
1
|
0.2
|
|
|
|
|
|
|
54
|
56
|
2
|
0.8
|
|
|
|
|
|
|
70
|
71
|
1
|
0.3
|
|
|
|
|
|
|
75
|
81
|
6
|
2.7
|
|
|
Including
|
|
|
|
75
|
78
|
1
|
10.8
|
|
|
|
|
|
|
87
|
89
|
2
|
0.6
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0006
|
-60
|
225
|
111
|
9
|
11
|
2
|
0.4
|
|
|
|
|
|
|
19
|
20
|
1
|
0.9
|
|
|
|
|
|
|
32
|
33
|
1
|
0.5
|
|
|
|
|
|
|
51
|
52
|
1
|
0.3
|
|
|
|
|
|
|
51
|
59
|
8
|
1.3
|
|
|
Including
|
|
|
|
55
|
57
|
2
|
4.6
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0007
|
-60
|
225
|
90
|
82
|
83
|
1
|
4.2
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0008
|
-60
|
225
|
90
|
23
|
24
|
1
|
0.9
|
|
|
|
|
|
|
32
|
33
|
1
|
1.0
|
|
|
MTRC0009
|
-60
|
225
|
90
|
0
|
5
|
5
|
0.9
|
|
|
Including
|
|
|
|
2
|
4
|
2
|
1.8
|
|
|
|
|
|
|
25
|
26
|
1
|
0.3
|
|
|
|
|
|
|
29
|
30
|
1
|
0.6
|
|
|
|
|
|
|
59
|
78
|
19
|
1.3
|
|
|
Including
|
|
|
|
59
|
61
|
2
|
4.8
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0010
|
-60
|
225
|
84
|
30
|
31
|
1
|
0.2
|
|
|
|
|
|
|
32
|
33
|
1
|
0.2
|
|
|
|
|
|
|
52
|
53
|
1
|
0.2
|
|
|
MTRC0011
|
-60
|
225
|
72
|
18
|
19
|
1
|
0.2
|
|
|
|
|
|
|
31
|
33
|
2
|
11.8
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0012
|
-60
|
225
|
78
|
68
|
72
|
4
|
0.6
|
|
|
Including
|
|
|
70
|
70
|
71
|
1
|
1.3
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0013
|
-60
|
225
|
93
|
12
|
13
|
1
|
0.4
|
|
|
|
|
|
|
19
|
21
|
2
|
0.6
|
|
|
|
|
|
|
60
|
62
|
2
|
0.4
|
|
|
|
|
|
|
68
|
72
|
4
|
0.4
|
|
|
|
|
|
|
77
|
82
|
5
|
0.8
|
|
|
|
|
|
|
84
|
87
|
3
|
0.2
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0014
|
-60
|
225
|
102
|
18
|
35
|
17
|
1.6
|
|
|
Including
|
|
|
|
31
|
33
|
2
|
11.3
|
|
|
|
|
|
|
39
|
44
|
5
|
1.7
|
|
|
Including
|
|
|
|
41
|
43
|
1
|
4.3
|
|
|
|
|
|
|
62
|
65
|
3
|
1.1
|
|
|
|
|
|
|
71
|
72
|
1
|
0.3
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0015
|
-60
|
225
|
99
|
25
|
41
|
16
|
0.4
|
|
|
|
|
|
|
40
|
41
|
1
|
1.4
|
|
|
Including
|
|
|
|
51
|
52
|
1
|
17.0
|
|
|
|
|
|
|
60
|
74
|
14
|
0.3
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0016
|
-60
|
225
|
102
|
36
|
39
|
3
|
1.8
|
|
|
Including
|
|
|
|
38
|
39
|
1
|
5.1
|
|
|
|
|
|
|
66
|
67
|
1
|
2.9
|
|
|
|
|
|
|
85
|
86
|
1
|
0.4
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0017
|
-60
|
225
|
90
|
61
|
64
|
3
|
2.0
|
|
|
|
|
|
|
69
|
71
|
2
|
0.2
|
|
|
|
|
|
|
75
|
76
|
1
|
0.5
|
|
|
|
|
|
|
78
|
85
|
7
|
0.4
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0018
|
-60
|
225
|
90
|
9
|
11
|
2
|
0.3
|
|
|
|
|
|
|
18
|
21
|
3
|
0.8
|
|
|
|
|
|
|
34
|
35
|
1
|
0.7
|
|
|
|
|
|
|
45
|
47
|
2
|
0.3
|
|
|
|
|
|
|
55
|
56
|
1
|
0.3
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0019
|
-60
|
225
|
84
|
|
|
|
NSR
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0020
|
-60
|
225
|
87
|
41
|
43
|
2
|
1.6
|
|
|
|
|
|
|
53
|
54
|
1
|
0.3
|
|
|
|
|
|
|
60
|
70
|
10
|
1.2
|
|
|
Including
|
|
|
|
60
|
66
|
1
|
8.9
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0021
|
-90
|
0
|
30
|
84
|
92
|
8
|
0.7
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0022
|
-50
|
125
|
51
|
17
|
28
|
11
|
8.6
|
|
|
Including
|
|
|
|
24
|
27
|
3
|
30.9
|
|
|
|
|
|
|
44
|
45
|
1
|
0.3
|
|
|
|
|
|
|
|
|
|
|
|
|
MTRC0023
|
-60
|
10
|
55
|
22
|
24
|
2
|
0.9
|
|
SOURCE Tajiri Resources Corp.