TORONTO, Sept. 10, 2019 /CNW/ - PowerOre Inc.
("Power Ore" or the "Company") (TSX.V: PORE) is pleased to report
its detailed summary of the results including plans, sections and
interpratations from its recent 2019 drill program at the
Opemiska Copper Mine Complex ("Opemiska") in the Chibougamau District of Quebec. Opemiksa consists of two former
producing underground mines, Springer and Perry. This drill program
focused exclusively on Springer which is being reinterpreted as an
open pit project.
Power Ore's conclusion from the drill program:
- Confirmation of our hypothesis for near surface disseminated
mineralization with twelve mineralized intersections over or near
100 metres;
- Further drilling is needed in areas where mineralization was
previously not expected, specifically in the Hinge Zone within the
rhyolite, previously interpreted as barren and the Southeast Zone
which delivered a 284 metre mineralized interval;
- Further drilling is needed on newly discovered high grade veins
outside of the previously mined envelope;
- Crown Pilars are thicker than anticipated
Notable intersections from Opemiska's 23 hole, 3,364 metre
drill program include:
High-grade Intersections with Copper Eq* over 1.00%
Copper Eq
(%)*
|
Interval
(m)
|
From
(m)
|
To
(m)
|
Hole
ID
|
Zone
|
4.65
|
7.9
|
81.1
|
89.0
|
OPM-19-19
|
Mill
|
4.15
|
25.0
|
38.0
|
63.0
|
OPM-19-18
|
Mill
|
3.07
|
43.0
|
38.0
|
81.0
|
OPM-19-14
|
Hinge
|
2.54
|
74.0
|
28.0
|
102.0
|
OPM-19-18
|
Mill
|
2.12
|
11.9
|
49.4
|
61.3
|
OPM-19-02
|
Hinge
|
1.96
|
19.0
|
81.0
|
100.0
|
OPM-19-13
|
Hinge
|
1.79
|
13.8
|
94.2
|
108.0
|
OPM-19-09
|
Southeast
|
1.76
|
5.5
|
51.0
|
56.5
|
OPM-19-06
|
Mill
|
1.62
|
14.8
|
61.5
|
76.3
|
OPM-19-20
|
Mill
|
1.55
|
7.0
|
18.0
|
25.0
|
OPM-19-20
|
Mill
|
1.52
|
26.0
|
76.0
|
102.0
|
OPM-19-22
|
Mill
|
1.39
|
10.0
|
141.0
|
151.0
|
OPM-19-16
|
Hinge
|
1.19
|
7.9
|
14.2
|
22.1
|
OPM-19-07
|
Mill
|
1.17
|
13.0
|
97.0
|
110.0
|
OPM-19-07
|
Mill
|
1.16
|
5.7
|
53.0
|
58.7
|
OPM-19-03
|
Hinge
|
1.10
|
15.3
|
34.0
|
49.3
|
OPM-19-21
|
Hinge
|
1.09
|
23.8
|
7.2
|
31.0
|
OPM-19-04
|
Mill
|
1.01
|
162.0
|
3.0
|
165.0
|
OPM-19-14
|
Hinge
|
Mineralized Intervals near or over 100 metres
Copper Eq
(%)*
|
Interval
(m)
|
From
(m)
|
To
(m)
|
Hole
ID
|
Zone
|
0.30
|
284.4
|
27.6
|
312.0
|
OPM-19-09
|
Southeast
|
0.20
|
224.5
|
2.0
|
226.5
|
OPM-19-06
|
Mill
|
0.22
|
186.0
|
6.0
|
192.0
|
OPM-19-04
|
Mill
|
1.01
|
162.0
|
3.0
|
165.0
|
OPM-19-14
|
Hinge
|
0.35
|
137.9
|
12.1
|
150.0
|
OPM-19-13
|
Hinge
|
0.65
|
133.9
|
16.1
|
150.0
|
OPM-19-19
|
Mill
|
0.32
|
130.6
|
9.0
|
139.6
|
OPM-19-07
|
Southeast/Mill
|
0.48
|
114.0
|
36.0
|
150.0
|
OPM-19-22
|
Mill
|
0.27
|
113.4
|
0.6
|
114.0
|
OPM-19-01
|
Hinge
|
0.76
|
105.0
|
2.0
|
107.0
|
OPM-19-02
|
Hinge
|
0.36
|
100.0
|
7.0
|
107.0
|
OPM-19-21
|
Hinge
|
0.56
|
97.0
|
55.0
|
152.0
|
OPM-19-16
|
Hinge
|
*Copper Equivalent ("Cu Eq.") grade including copper, gold,
silver, cobalt and zinc based on 100% recoveries is calculated
using the following equation: Cu Eq. = [(Cu % x 20 x Cu price) +
(Au grade / 34.2857 x Au price) + (Ag grade / 34.2857 x Ag price) +
(Co % x 20 x Co price) + (Zn % x 20 x Zn price)] / (20 x Cu price).
We used Cu, Au, Ag, Co and Zn price of US$2.65, US$1,400
and US$14.75, US$15.00 and US$1.19 respectively.
Click here for Plan Views and Sections from
Recent Drill Program
Click here for Map of Drill Hole Locations and
Zones
Zones of Exploration on Springer from Recent Drill
Program
Hinge Zone
Holes 11 to 16 and 21 were
drilled on either side of the glory hole of #3 Vein and in the
vicinity of the crown pillars of #1 and #2 veins to test for
dissiminated mineralization along the rhyolite-pyroxenite/gabbro
contact in the hinge zone of the regional fold. The twinned
hole 01, was also drilled in the Hinge Zone and confirms
mineralization previously drilled by Falconbridge. Holes 02, 03 and 11 confirmed
that much low grade material was left behind from mining of the
glory hole and indicate that the disseminated mineralization
extends for at least 175 metres perpendicular from the contact with
rhyolite. The drilling also showed that the rhyolite can be
mineralized as shown in Hole 03, drilled entirely in the rhyolite
and intersecting 0.35% Cu-EQ* over 58.0 metres. Moreover the
drilling highlighted a number narrow high-grade veins that were
never mined and as such were never identified by Falconbridge. Holes 02, 14 and 16 were notable
holes in this zone, with Hole 02 intersecting 0.76% CuEq over 105.0
metres, Hole 14 intersecting 1.01% CuEq over 162.0 metres and Hole
16 intersecting 0.56% CuEq over 97.0 metres.
Mill Zone
The Mill Zone is located along the
rhyolite-pyroxenite/gabbro contact and extends towards the
northeast from the Hinge Zone. Holes 18, 20 and 22 were all
oriented northwest and drilled into the rhyolite contact whereas
Hole 19 was drilled to the south and collared between the Mill Zone
and the Hinge Zone. The Mill Zone represents deep crown pillars
under the old mill and abundant disseminated mineralization in the
Ventures gabbro between #20 and #23 veins and extends to the south
towards #1 Vein. The drilling confirms high grades of the
disseminated mineralization with Hole 18 intersecting 2.54% Cu-EQ*
over 74.0 metres and the thick and very high grades of the crown
pillars of #20 Vein (4.15% Cu-EQ* over 25.0 metres from 38.0 metres
in Hole 18), of #1 Vein (4.65% Cu-EQ* over 7.9 metres from 81.1
metres in Hole 19) and of #3 Vein (1.52% Cu-EQ* over 26.0 metres
from 76.0 metres in Hole 22).
Southeast Zone
Only Hole 09 (a twinned hole) was
drilled into the Southeast Zone. This area is to the south of
#3 Vein and extends to the south to #7 Vein and from the glory hole
to the abandoned railway spur. Hole 09 intersected 0.30% Cu-EQ*
over 284.4 metres.
Gold Potential of Opemiska Property
Gold was an
important by-product from the Springer Mine. At mine closure,
Falconbridge (Minnova at the time)
reported in situ reserves at Springer totaling 2.44 million tonnes
grading 1.67% copper and 1.89 gpt gold (see note on historical
mineral reserves and mineral resources at the end of this news
release).
A total of 1135 samples of half core were analysed for gold in
addition to copper, silver, cobalt and zinc. The average content of
gold, which is 0.18 gpt gold, is more influenced by the high
outlier values of gold among the samples. Although no
systematic spatial relationship has been identified for the high
gold values, there is good correlation between gold and copper,
with nearly 5% of the gold assays showing over 1.0 gpt gold (with
the highest value of 9.87 gpt gold). Additionally, historical
reports while the Springer underground mine was operational make
reference to the Arsenopyrite vein which occurs behind the old
mill. This vein was reported to contain generally low copper
values, which is why it was never mined, but contained elevated
gold values. At the generally prevailing gold prices during most of
Springer's mine life (1956-1991), this type of vein would not have
been attractive to the mine, given they had a floatation mill which
is unsuitable for gold associated with arsenopyrite.
Exploration Holes
Drill holes 02, 03, 06, and holes 10
to 23 are all exploration holes and were mainly drilled to fill
gaps between Falconbridge surface
drill holes to get a better understading of the dissiminated
mineralization and complete the Springer block model with more
accuracy.
Twinned Holes
Holes 01, 04, 05, and 07 to 09 were
twins of holes drilled by Falconbridge to validate the extensive surface
and underground historical drilling (800,000 metres) previously
conducted by Falconbridge at
Opemiska during its past exploration and underground production
stages. We note that given that a significant amount of drilling
occurred while Opemiska was in production under Falconbridge, reconciliation of tonnage and
grade occurred annually and hence, attests to the high quality of
this historical data. Once validated, the historical data can be
used as part of a resource estimate at
Opemiska.
Principal Conclusions
This first phase of drilling on
the historical Springer Mine has confirmed our expectations
regarding the distribution of disseminated mineralization, while
posing new questions regarding distribution of the mineralization
and new mineralized areas previously interpreted to be
unmineralized. Mineralization increases closer to the
rhyolite-pyroxenite/gabbro contact, and we see better than expected
mineralization south of #3 Vein, towards #7 Vein. The
footwall rhyolite was also found to be more mineralized than
expected and the disseminated material in the Mill Zone in the
vicinity of #20 and #23 veins is much better than expected, with
the crown pillars thicker than expected. Finally, it should be
noted that no drilling was done on Perry, which still had
significant underground reserves remaining when the mine shutdown
in 1991 and for which RPA estimated underground exploration targets
between 3.0 and 11.0 million tonnes at between 1.5% and 2.5% copper
(see note on Exploration Targets at the end of this news
release).
Next Steps
Springer
It is clear that
additional drilling is warranted in multiple existing and new
zones, in particular to redefine the limit of the rhyolite and
pyroxenite/gabbro and Southeast zones. Additionally, further infill
drilling is required to increase the confidence in resource
estimate categorization.
Perry
Digitizing of historical work and generation of
a block model digitizing is expected to be complete in September.
Once complete, its geologic model will be on par with that of
Springer. This will allow the Company to complete its internal
resource estimate and to define targets for its ensuing drill
program.
A detailed future work plan for Perry and Spring will follow in
a subsequent news release.
Orientation of Drilling and True Widths of
Mineralization
Field based and drill hole evidence clearly
indicate that several orientations of veins are present on the
Opemiska Property but that around the Springer Mine the veins are
predominantly EW with a steep dip to the north. South
directed drill holes are intersecting those veins near
perpendicular. However in the disseminated mineralization we
find veins with various core angles suggesting that other
directions may be important. As such, in the disseminated
mineralization the true width of mineralized intersections is
estimated to be the same as the drill core width even though the
mineralization may have an overall envelope that is different.
QP Statement
The technical information contained in
this news release has been reviewed and approved by Charles Beaudry, P.Geo and géo., Director
and Vice President Exploration for Power Ore, who is a Qualified
Person as defined in "National Instrument 43-101, Standards of
Disclosure for Mineral Projects." For the exploration
undertaken by Power Ore all assay batches are accompanied by
rigorous Quality Assurance procedures that include insertion of
standards and blanks and verification assays in a secondary
laboratory. Quality Control results, including the
laboratory's own control samples, are evaluated immediately on
reception of batch results and corrections implemented immediately
if necessary. All drill collars are surveyed and positioned
in UTM coordinates. Downhole deviations surveys are done with
a Reflex instrument at 30m
intervals. A systematic density measurement program using two
methods was implemented to measure density of all rock types.
A specific susceptibility measurement protocol was also implemented
to better estimate the relative abundance of magnetite in the
variably magnetic rocks of the Ventures Sill.
Note on Historical Mineral Reserves and Mineral Resources and
on Exploration Targets
The mineral reserves left in the mine
when production was suspended are historical in nature and cannot
be considered mineral reserves for our purposes. Power Ore
considers that insufficient work has been done on the Springer mine
to define any mineral resources and does consider historical
reserves to be mineral reserves or mineral resources and only
presents these numbers to indicate the amount of mineralized
material left behind by Falconbridge. The potential tonnage
and grade of Exploration Targets defined by RPA Consultants are
conceptual in nature. There has been insufficient exploration
to define them as mineral resources and it is uncertain if further
exploration will result in the targets being delineated as mineral
resources. As such Power Ore does not consider exploration
targets as mineral resources and neither should the reader.
About Opemiska Copper Mine Complex
The Opemiska Copper
Complex is located adjacent to the town of Chapais, Quebec within the Chibougamau region. Opemiska is also within
the Abitibi Greenstone belt and within the boundaries of the
Province of Quebec's Plan Nord
which promotes and funds infrastructure and development of natural
resource projects. The project consists of 11 mining claims and
covers the past producing Springer & Perry mines which were
owned and operated by Falconbridge. The project has excellent in
place infrastructure including a powerstation and direct access to
Highway 113 and the Canadian National Railway.
Opemiska was mined by Falconbridge as a high-grade underground
mining operation and was in production for over 35 years prior to
Ex-In acquiring the property in 1993.
For information and updates on Power Ore, please
visit: www.powerore.com
And please follow us on Twitter @PowerOre
Neither 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. Certain information in this press release may contain
forward-looking statements. This information is based on current
expectations that are subject to significant risks and
uncertainties that are difficult to predict. Actual results might
differ materially from results suggested in any forward-looking
statements. Power Ore is a trade name of PowerOre Inc. PowerOre
Inc. assumes no obligation to update the forward-looking
statements, or to update the reasons why actual results could
differ from those reflected in the forward looking-statements
unless and until required by securities laws applicable to PowerOre
Inc. Additional information identifying risks and uncertainties is
contained in filings by PowerOre Inc. with Canadian securities
regulators, which filings are available under PowerOre Inc. profile
at www.sedar.com.
Table 1: Summary statistics of spring 2019 diamond
drilling program on Opemiska Project. Note that collars have
not yet been surveyed.
HOLE_ID
|
UTEM_EAST
|
UTM_NORTH
|
AZIMUTH
|
DIP
|
DATE_STARTED
|
DATE_ENDED
|
OVERBURDEN
|
LENGTH_M
|
CUMMULATIVE_M
|
OPM-19-01
|
509620.0
|
5515006.0
|
180
|
-48
|
May
16/2019
|
May17/2019
|
1.3
|
139.1
|
139.1
|
OPM-19-02
|
509668.0
|
5515069.0
|
180
|
-50
|
May
17/2019
|
May
18/2019
|
2.0
|
107.5
|
246.6
|
OPM-19-03
|
509510.0
|
5514950.0
|
180
|
-60
|
May
18/2019
|
May
19/2019
|
2.6
|
115.4
|
362.0
|
OPM-19-04
|
509880.0
|
5514959.0
|
180
|
-47
|
May
19/2019
|
May
20/2019
|
3.0
|
193.7
|
555.7
|
OPM-19-05
|
509805.0
|
5514939.0
|
180
|
-46
|
May
20/2019
|
May
21/2019
|
2.5
|
98.5
|
654.2
|
OPM-19-06
|
509830.0
|
5515009.0
|
180
|
-50
|
May 21/
2019
|
May
23/2019
|
2.5
|
226.5
|
880.7
|
OPM-19-07
|
509778.0
|
5514820.0
|
180
|
-48
|
May 23/
2019
|
May 24/
2019
|
2.3
|
139.6
|
1020.3
|
OPM-19-08
|
509957.0
|
5514963.0
|
180
|
-45
|
May 24/
2019
|
May
25/2019
|
2.0
|
188.0
|
1208.3
|
OPM-19-09
|
510066.0
|
5514786.0
|
180
|
-65
|
May 24/
2019
|
May 28
/2019
|
8.0
|
320.6
|
1528.9
|
OPM-19-10
|
509975.0
|
5514896.0
|
180
|
-49
|
May 28/
2019
|
May
28/2019
|
3.0
|
51.1
|
1580.0
|
OPM-19-11
|
509592.0
|
5514808.0
|
360
|
-60
|
May
29/2019
|
May
29/2019
|
12.5
|
37.9
|
1617.9
|
OPM-19-12
|
509592.0
|
5514808.0
|
225
|
-45
|
May
29/2019
|
May
31/2019
|
11.5
|
122.6
|
1740.5
|
OPM-19-13
|
509592.0
|
5514808.0
|
300
|
-45
|
May
31/2019
|
June 01/
2019
|
11.8
|
195.7
|
1936.2
|
OPM-19-14
|
509620.5
|
5515005.8
|
230
|
-45
|
June
01/2019
|
June 03/
2016
|
2.7
|
173.0
|
2109.2
|
OPM-19-15
|
509620.5
|
5515005.8
|
315
|
-45
|
June 03/
2019
|
June 03/
2019
|
17.7
|
38.0
|
2147.2
|
OPM-19-16
|
509640.0
|
5514904.0
|
315
|
-45
|
June 04/
2019
|
June
05/2019
|
2.5
|
160.5
|
2307.7
|
OPM-19-17
|
509668.0
|
5515068.8
|
315
|
-45
|
June
05/2019
|
June
05/2019
|
2.3
|
100.9
|
2408.6
|
OPM-19-18
|
509753.1
|
5515065.4
|
315
|
-45
|
June
06/2019
|
June
07/2019
|
2.8
|
146.9
|
2555.5
|
OPM-19-19
|
509753.0
|
5515040.0
|
180
|
-45
|
June 07/
2019
|
June
08/2019
|
1.2
|
158.3
|
2713.8
|
OPM-19-20
|
509790.0
|
5515124.0
|
315
|
-45
|
June
08/2019
|
June 09/
2019
|
6.7
|
149.0
|
2862.8
|
OPM-19-21
|
509671.0
|
5514936.0
|
180
|
-60
|
June
09/2019
|
June
10/2019
|
1.4
|
113.6
|
2976.4
|
OPM-19-22
|
509835.0
|
5515145.0
|
315
|
-45
|
June
10/2019
|
June
11/2019
|
1.7
|
150.0
|
3126.4
|
OPM-19-23
|
509974.0
|
5515286.0
|
315
|
-45
|
June
11/2019
|
June
13/2019
|
5.7
|
223.6
|
3363.9
|
Table 2: Spring 2019 Drill Results from Springer
Hole
ID
|
Grade
|
Interval
(m)
|
From
(m)
|
To
(m)
|
Copper Eq
(%)
|
Copper
(%)
|
Gold
(gpt)
|
Silver
(gpt)
|
Cobalt
(%)
|
Zinc
(%)
|
OPM-19-01
|
0.27
|
0.15
|
0.09
|
1.43
|
0.005
|
0.03
|
113.4
|
0.60
|
114.0
|
Including*
|
0.98
|
0.50
|
0.41
|
5.93
|
0.006
|
0.19
|
15.0
|
51.0
|
66.0
|
and*
|
0.39
|
0.25
|
0.12
|
1.74
|
0.005
|
0.005
|
9.20
|
96.8
|
106.0
|
|
|
|
|
|
|
|
|
|
|
OPM-19-02
|
0.76
|
0.43
|
0.36
|
2.72
|
0.005
|
0.02
|
105.0
|
2.0
|
107.0
|
Including*
|
2.12
|
1.81
|
0.22
|
10.6
|
0.005
|
0.074
|
11.9
|
49.4
|
61.3
|
and*
|
5.60
|
2.53
|
3.66
|
14.8
|
0.016
|
0.093
|
8.00
|
99.0
|
107.0
|
|
|
|
|
|
|
|
|
|
|
OPM-19-03
|
0.35
|
0.22
|
0.84
|
5.02
|
0.002
|
0.028
|
58.0
|
33.0
|
91.0
|
Including*
|
1.16
|
0.71
|
0.35
|
14.2
|
0.007
|
0.06
|
5.7
|
53.0
|
58.7
|
|
|
|
|
|
|
|
|
|
|
OPM-19-04
|
0.22
|
0.13
|
0.10
|
1.03
|
0.002
|
0.009
|
186.0
|
6.00
|
192.0
|
Including*
|
1.09
|
0.53
|
0.61
|
5.48
|
0.005
|
0.045
|
23.8
|
7.2
|
31.0
|
and*
|
1.79
|
1.50
|
0.21
|
6.39
|
0.008
|
0.059
|
4.30
|
186.6
|
190.9
|
|
|
|
|
|
|
|
|
|
|
OPM-19-05^
|
2.17
|
0.84
|
1.54
|
9.1
|
0.010
|
0.027
|
2.4
|
96.1
|
98.5
|
|
|
|
|
|
|
|
|
|
|
OPM-19-06
|
0.20
|
0.12
|
0.078
|
0.86
|
0.002
|
0.012
|
224.5
|
2.00
|
226.5
|
Including*
|
1.76
|
1.30
|
0.49
|
5.41
|
0.005
|
0.030
|
5.50
|
51.0
|
56.5
|
|
|
|
|
|
|
|
|
|
|
OPM-19-07
|
0.32
|
0.18
|
0.16
|
0.94
|
0.002
|
0.003
|
130.6
|
9.00
|
139.6
|
Including*
|
1.19
|
0.84
|
0.32
|
6.74
|
0.008
|
0.011
|
7.90
|
14.2
|
22.1
|
and*
|
1.17
|
0.39
|
0.99
|
1.22
|
0.002
|
0.002
|
13.0
|
97.0
|
110.0
|
|
|
|
|
|
|
|
|
|
|
OPM-19-08
|
0.52
|
0.35
|
0.12
|
3.31
|
0.004
|
0.08
|
12.4
|
116.6
|
129.0
|
|
|
|
|
|
|
|
|
|
|
OPM-19-09
|
0.30
|
0.20
|
0.10
|
1.09
|
0.003
|
0.008
|
284.4
|
27.6
|
312.0
|
Including*
|
0.77
|
0.59
|
0.15
|
3.41
|
0.005
|
0.009
|
19.6
|
26.4
|
46.0
|
and*
|
1.79
|
1.45
|
0.33
|
4.43
|
0.008
|
0.014
|
13.8
|
94.2
|
108.0
|
and*
|
0.33
|
0.24
|
0.07
|
0.84
|
0.003
|
0.003
|
13.4
|
122.0
|
135.4
|
and*
|
1.03
|
0.56
|
0.46
|
4.97
|
0.01
|
0.08
|
16.0
|
296.0
|
312.0
|
|
|
|
|
|
|
|
|
|
|
OPM-19-10
|
No significant
intersection
|
|
|
|
|
|
|
|
|
|
|
OPM-19-11*
|
0.73
|
0.48
|
0.25
|
4.49
|
0.003
|
0.02
|
14.8
|
19.20
|
34.00
|
|
|
|
|
|
|
|
|
|
|
OPM-19-12*
|
0.43
|
0.25
|
0.17
|
2.11
|
0.005
|
0.01
|
14.0
|
12.00
|
26.00
|
|
|
|
|
|
|
|
|
|
|
OPM-19-13
|
0.35
|
0.26
|
0.08
|
1.14
|
0.004
|
0.008
|
137.9
|
12.10
|
150.0
|
Including*
|
1.96
|
1.51
|
0.46
|
5.07
|
0.008
|
0.013
|
19.0
|
81.0
|
100.0
|
|
|
|
|
|
|
|
|
|
|
OPM-19-14
|
1.01
|
0.46
|
0.20
|
3.68
|
0.003
|
0.79
|
162.0
|
3.00
|
165.0
|
Including*
|
3.07
|
1.27
|
0.56
|
8.78
|
0.005
|
2.82
|
43.0
|
38.0
|
81.0
|
and*
|
0.54
|
0.15
|
0.19
|
2.28
|
0.004
|
0.447
|
8.0
|
89.0
|
97.0
|
|
|
|
|
|
|
|
|
|
|
OPM-19-15*
|
0.39
|
0.28
|
0.10
|
0.78
|
0.004
|
0.007
|
16.0
|
19.0
|
35.0
|
|
|
|
|
|
|
|
|
|
|
OPM-19-16
|
0.56
|
0.35
|
0.21
|
2.48
|
0.004
|
0.009
|
97.0
|
55.0
|
152.0
|
Including*
|
0.72
|
0.41
|
0.34
|
3.05
|
0.004
|
0.011
|
50.0
|
55.00
|
105.0
|
and*
|
1.39
|
1.13
|
0.24
|
6.48
|
0.003
|
0.008
|
10.0
|
141.0
|
151.0
|
|
|
|
|
|
|
|
|
|
|
OPM-19-17^
|
1.13
|
0.81
|
0.34
|
3.20
|
0.004
|
0.008
|
2.00
|
18.00
|
20.00
|
|
|
|
|
|
|
|
|
|
|
OPM-19-18
|
2.54
|
2.13
|
0.41
|
7.61
|
0.006
|
0.013
|
74.0
|
28.0
|
102.0
|
Including*
|
4.15
|
3.25
|
0.96
|
11.3
|
0.01
|
0.02
|
25.0
|
38.0
|
63.0
|
and*
|
5.40
|
4.95
|
0.33
|
18.0
|
0.008
|
0.024
|
14.5
|
73.0
|
87.5
|
|
|
|
|
|
|
|
|
|
|
OPM-19-19
|
0.65
|
0.53
|
0.11
|
1.82
|
0.003
|
0.008
|
133.9
|
16.10
|
150.0
|
Including*
|
0.59
|
0.47
|
0.11
|
1.34
|
0.003
|
0.005
|
13.2
|
16.1
|
29.3
|
and*
|
4.65
|
4.10
|
0.51
|
11.15
|
0.008
|
0.018
|
7.90
|
81.1
|
89.0
|
and*
|
0.52
|
0.37
|
0.16
|
1.46
|
0.004
|
0.005
|
19.0
|
98.6
|
117.6
|
and*
|
1.82
|
1.51
|
0.27
|
7.01
|
0.006
|
0.017
|
12.3
|
137.7
|
150.0
|
|
|
|
|
|
|
|
|
|
|
OPM-19-20
|
0.57
|
0.41
|
0.15
|
2.02
|
0.003
|
0.006
|
102.1
|
15.0
|
117.1
|
Including*
|
1.55
|
1.27
|
0.24
|
8.06
|
0.004
|
0.011
|
7.00
|
18.0
|
25.0
|
and*
|
1.62
|
1.07
|
0.61
|
5.07
|
0.006
|
0.011
|
14.8
|
61.5
|
76.3
|
and*
|
0.97
|
0.77
|
0.19
|
2.87
|
0.005
|
0.010
|
21.1
|
96.0
|
117.1
|
|
|
|
|
|
|
|
|
|
|
OPM-19-21
|
0.36
|
0.17
|
0.20
|
1.57
|
0.003
|
0.009
|
100.0
|
7.00
|
107.0
|
Including*
|
0.50
|
0.37
|
0.10
|
2.34
|
0.003
|
0.008
|
17.0
|
7.00
|
24.0
|
and*
|
1.10
|
0.27
|
1.00
|
3.76
|
0.003
|
0.011
|
15.3
|
34.0
|
49.3
|
|
|
|
|
|
|
|
|
|
|
OPM-19-22
|
0.48
|
0.34
|
0.14
|
1.13
|
0.003
|
0.004
|
114.0
|
36.0
|
150.0
|
Including*
|
1.52
|
1.11
|
0.47
|
2.79
|
0.005
|
0.007
|
26.0
|
76.0
|
102.0
|
|
|
|
|
|
|
|
|
|
|
OPM-19-23
|
0.48
|
0.39
|
0.07
|
2.00
|
0.004
|
0.006
|
22.0
|
187.0
|
209.0
|
*: Composite includes intervals no greater than 6.0m with results inferior to 0.30% Cu-Eq.
^: Single sample composite.
SOURCE Power Ore