VANCOUVER, Sept. 5, 2019 /PRNewswire/ - Tinka Resources
Limited ("Tinka" or the "Company") (TSXV &
BVL: TK) (OTCPK: TKRFF) is pleased to announce assay
results for two recent holes drilled at the Company's 100%-owned
Ayawilca Property in central Peru.
Drilling is continuing with one rig operating at the South Ayawilca
area, with the focus on expanding and upgrading the high-grade
'Zinc Zone' mineralization as defined in the Company's recent
Preliminary Economic Assessment (PEA).
Hole A19-163 intercepted two intervals of high grade zinc
mineralization close to the margin of the current inferred
resource. The hole intersected one of the highest grade intervals
ever drilled at South Ayawilca. In addition, a new style of
silver-rich mineralization with disseminated zinc - lead was
intersected deeper in hole A19-163 within a down-faulted limestone
more than 100 metres beneath the current resource, with
mineralization remaining open to the west and at depth. The
footprint of the mineralization at Ayawilca continues to expand,
and still offers exciting exploration upside.
Key Highlights from hole A19-163:
Zinc Zone:
- 34.7 metres grading 6.7% zinc, 11 g/t silver and 86 g/t
indium from 171.0 metres, including
-
- 5.7 metres grading 9.7% zinc, 12 g/t silver and 147 g/t
indium from 199.1 metres; and
- 5.7 metres grading 32.6% zinc, 20 g/t silver and 89 g/t
indium from 228.0 metres; and
Lower Silver Zone:
- 13.9 metres grading 1.0% zinc, 0.6% lead and 128 g/t
silver from 397.7 metres, including
-
- 0.6 metres grading 5.4% zinc, 3.5% lead and 818 g/t
silver from 397.7 metres depth.
Note: True thicknesses of the Zinc Zone intersections are
estimated to be at least 85% of the downhole thicknesses. The true
thickness of the Lower Silver Zone intersection cannot be
determined at this time as insufficient data is available.
Recent drilling has significantly advanced the geological model
and understanding of the geometry of the high grade zinc
mineralization at the western end of South Ayawilca. The second
hole reported here, A19-164, was drilled up-dip from hole A19-163
at a shallower angle (50 degree dip) to test for extensions of the
existing zinc mineral resource but did not encounter
mineralization. A19-164 is interpreted to have drilled into the
roof zone of a hinge of an anticline fold, the core of which hosts
very high grade mineralization in multiple lenses or 'mantos',
including those intercepted in A19-163.
Dr. Graham Carman, Tinka's
President and CEO, stated: "The ongoing drill program at South
Ayawilca is focused on the expansion and upgrading of high-grade
resources in the Zinc Zone. We are excited that new drill holes
like A19-163 continue to intersect exceptional zinc grades.
The recently completed PEA shows that the project economics is
sensitive to zinc grade, so expansions or upgrading of these higher
grade zinc resources will have a positive impact on the project
economics in future studies."
"With the discovery of the Lower Silver Zone in hole A19-164,
we have proven that mineralization exists within a deeper limestone
at South Ayawilca, 100 to 150 metres beneath the existing resource,
open to the west and at depth. The Lower Silver Zone so far
consists of disseminated sulphides hosted in strongly altered
limestone where the original rock has been almost completely
replaced by iron - manganese carbonates, a style of mineralization
and alteration that had previously been encountered only in vein
form around the edges of the massive sulphide mineralization.
Further drilling is planned for the Lower Silver Zone, including
the deepening of a 2017 drill hole (A19-167) which is currently in
progress. Holes A19-165 and 166 were recently completed and
assays are pending."
Discussion –Geological Model Updated
This release presents results for two new holes from South
Ayawilca (A19-163 and A19-164). Hole A19-163 intersected two
high grade intervals of zinc mineralization on the edge of the
existing mineral resource between 170 and 240 metres depth (see
Figure 1). The zinc intercepts in this hole consist of
reddish-coloured massive sphalerite (see Figure 2), a style of zinc
mineralization with relatively low iron.
The Lower Silver Zone mineralization in hole A19-163 is hosted
by recrystallized and altered limestone at approximately 400 metres
depth, separated from the Zinc Zone resource by a reverse fault
(the Colquipucro Fault system – see Figures 1 & 3). The fault
displacement is believed to be post-mineral, so the downthrown
western fault block could host extensions of the high-grade zinc
mineralization as well as the silver-rich mineralization.
Hole A19-164 did not intersect significant mineralization up-dip
from A19-163, and is interpreted to have remained in the barren
roof zone of a tightly folded anticline structure (Figure
1).
The 2019 drilling has highlighted several complexities in the
structure of the Ayawilca deposit, which is assisting us greatly in
understanding the controls and distribution of the high grade
mineralization. A shallow east-dipping contact between phyllite and
limestone is interpreted to be an early low-angle thrust fault
which pre-dates mineralization. The thrust fault was important in
the preparation of the host rocks (brecciation) and likely occurred
at the same time as the anticline folding. These low angle
structures acted as feeders for the zinc mineralization and the
anticline fold acted as a structural trap. Some of the highest
grades encountered at Ayawilca are found within the limestone core
of the anticline.
The mineralization is interpreted to be displaced by the
post-mineral Colquipucro Fault, with a possible offset of at least
100-150 metres vertically, with additional unknown lateral
displacement. The Lower Silver Zone mineralization occurs
within this downthrown block, and remains open and untested to the
west.
Table 1 – Summary of new drill holes assays from
Ayawilca
Hole
|
From
(m)
|
To
(m)
|
Interval
(m)
|
Zn
%
|
Pb
%
|
Ag
ppm
|
In
ppm
|
A19-163
|
118.80
|
120.05
|
1.25
|
25.58
|
0.01
|
33
|
243
|
and
|
171.00
|
205.70
|
34.70
|
6.68
|
0.10
|
11
|
86
|
incl
|
199.10
|
204.80
|
5.70
|
9.71
|
0.01
|
12
|
147
|
and
|
228.00
|
233.70
|
5.70
|
32.64
|
0.02
|
20
|
89
|
and
|
397.70
|
411.60
|
13.90
|
1.04
|
0.64
|
128
|
2
|
incl
|
397.70
|
398.30
|
0.60
|
5.43
|
3.45
|
818
|
1
|
A19-164
|
no significant
results
|
|
|
|
|
|
Note: True thicknesses of the zinc intersections in Table 1 are
estimated to be at least 85% of the downhole thicknesses as the
zinc mineralization at Ayawilca is generally flat-dipping
replacement of layers or 'mantos' hosted by limestone and/or
sandstone. The true thickness of the silver intersection
cannot be determined at this time as insufficient data is
available.
Table 2 – 2019 Drill Collar Information
(coordinates are in UTM Zone 18S WGS84
datum)
Hole
ID
|
Easting
|
Northing
|
Elevation
|
Azimuth
|
Dip
|
Depth
m
|
A19-163
|
333047
|
8845065
|
4197
|
260
|
-65
|
496.6
|
A19-164
|
333047
|
8845065
|
4197
|
260
|
-50
|
257.8
|
A19-165
|
333047
|
8845065
|
4197
|
280
|
-62
|
463.5
|
Notes on sampling and assaying
Drill holes are diamond HQ or NQ size core holes with recoveries
generally above 80% and often close to 100%. The drill core is
marked up, logged, and photographed on site. The cores are cut in
half at the Company's core storage facility, with half-cores stored
as a future reference. Half-core is bagged on average over 1 to 2
metre composite intervals and sent to ALS laboratories in
Lima for assay in batches.
Standards and blanks are inserted into each batch prior to
departure from Tinka's core storage facilities. At the laboratory
samples are dried, crushed to 100% passing 2mm, then 500 grams
pulverized for multi-element analysis by ICP using multi-acid
digestion. Samples assaying over 1% zinc, lead, or copper and over
100 g/t silver are re-assayed using precise ore-grade AAS
techniques.
Qualified Person
Dr. Graham Carman, Tinka's
President and CEO, reviewed, verified and compiled the technical
contents of this release. Dr Carman is a Fellow of the Australasian
Institute of Mining and Metallurgy, and is a qualified person as
defined by National Instrument 43-101.
About Tinka Resources Limited
Tinka is an exploration and development company with its
flagship property being the 100%-owned Ayawilca carbonate
replacement deposit (CRD) located in the zinc-lead-silver belt of
central Peru, 200 kilometres
northeast of Lima. The Ayawilca
Zinc Zone contains 11.7 Mt of Indicated Resources grading 6.9%
zinc, 0.2% lead, 15 g/t silver and 84 g/t indium and 45.0 Mt
Inferred Resources grading 5.6% zinc, 0.2% lead, 17 g/t silver and
67 g/t indium. The Ayawilca Tin Zone contains an Inferred
Mineral Resource of 14.5 Mt at 0.63% tin, 0.21% copper & 18 g/t
silver (November 26, 2018 release).
The Colquipucro silver oxide deposit contains 2.9 Mt of
Indicated Resources grading 112 g/t silver (for 10.4 Moz Ag) and 2.2 Mt Inferred Resources grading
105 g/t silver (for 7.5 Moz Ag) in
high grade lenses within a preliminary open pit shell using a
$46/t NSR cut off (November 26, 2018 release). A Preliminary
Economic Assessment for the Ayawilca Zinc Zone was released on
July 2, 2019 (see
release).
On behalf of the Board,
"Graham Carman"
Dr. Graham Carman, President &
CEO
Forward Looking Statements: Certain information in
this news release contains forward-looking statements and
forward-looking information within the meaning of applicable
securities laws (collectively "forward-looking
statements"). All statements, other than statements of
historical fact are forward-looking statements. Forward-looking
statements are based on the beliefs and expectations of Tinka as
well as assumptions made by and information currently available to
Tinka's management. Such statements reflect the current
risks, uncertainties and assumptions related to certain factors
including, without limitations, drilling results, the Company's
expectations regarding the Ayawilca Project PEA, capital and
other costs varying significantly from estimates, production rates
varying from estimates, changes in world metal markets, changes in
equity markets, uncertainties relating to the availability and
costs of financing needed in the future, equipment failure,
unexpected geological conditions, imprecision in resource estimates
or metal recoveries, success of future development initiatives,
competition, operating performance, environmental and safety risks,
delays in obtaining or failure to obtain necessary permits and
approvals from local authorities, community agreements and
relations, and other development and operating risks. Should any
one or more of these risks or uncertainties materialize, or should
any underlying assumptions prove incorrect, actual results may vary
materially from those described herein. Although Tinka
believes that assumptions inherent in the forward-looking
statements are reasonable, forward-looking statements are not
guarantees of future performance and accordingly undue reliance
should not be put on such statements due to the inherent
uncertainty therein. Except as may be required by applicable
securities laws, Tinka disclaims any intent or obligation to update
any forward-looking statement.
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 news release
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SOURCE Tinka Resources Limited