VANCOUVER, BC, Sept. 6,
2022 /CNW/ - Group Eleven Resources Corp. (TSXV: ZNG)
(OTC: GRLVF) (FRA: 3GE) ("Group Eleven" or the
"Company") is pleased to announce the discovery of
high-grade massive sulphides as part of an initial step-out
reconnaissance drill program at its 100%-interest Ballywire zinc
prospect ("Ballywire"), PG West Project ("PG West"),
Ireland.
Highlights:
- G11-468-03 intersected a broad zone of zinc-lead-silver
mineralization over a width of 66.0m, including four higher-grade
zones (true width estimated to be 80-100% of intercepted
width):
-
- 5.00m of 8.3% Zn+Pb (6.2% Zn
and 2.1% Pb) and 107 g/t Ag (starting at 228.2m downhole), including 2.03m of 18.8% Zn+Pb (13.9% Zn and 4.9% Pb) and
227 g/t Ag
- 6.85m of 15.4% Zn+Pb (11.1% Zn
and 4.3% Pb) and 160 g/t Ag (starting at 251.6m), including 2.05m of 40.8% Zn+Pb (30.5% Zn and 10.3% Pb) and
385 g/t Ag
- 1.71m of 12.2% Zn+Pb (10.3% Zn
and 1.9% Pb) and 38 g/t Ag (starting at 268.9m) and
- 0.96m of 5.1% Zn+Pb (4.4% Zn
and 0.8% Pb) and 15 g/t Ag (starting at 274.7m)
- The above intercepts contain several massive sulphide zones up
to 2.95m thick (downhole)
- This discovery hole represents a 410m step-out NE of G11-468-01 which
intersected 3.30m of 12.5% Zn+Pb (10.1% Zn and 2.4% Pb) and
48 g/t Ag (see news release dated September 7th, 2021)
- Discovery area around G11-468-03 remains
open and untested along strike for approximately 3km to
the ENE and 1.5km to the W, as well as, up-dip to the NNW for at
least 500m
- Immediate follow-up drilling is highly
warranted
"Given the large step-out, the wide zone of mineralization and
grades up to 52.4% Zn+Pb, G11-468-03 is one of the best
holes drilled in Ireland over
recent years. This fantastic result validates our team's hard work
building a robust geological understanding of our large license
area over the last several years," stated Bart Jaworski, CEO. "Ballywire is situated at
the intersection of the Pallas Green Corridor and the
south-westerly projection of the famous Rathdowney Trend,
which hosts the historic Lisheen and Galmoy zinc mines. Given the
above results and coupled with hole G11-468-01 drilled in 2021,
Ballywire is starting to exhibit signs of a large
system with high-grade zinc-lead mineralization now
pierced by three holes over approximately 1.5km. Exploration
upside remains wide open reflecting sparse historic
drilling. Notably, the next nearest historic hole to test the
target horizon to the ENE is 3km away, and yet still hosts an
appreciable 5.0m of 1.6% Zn+Pb."
"Unlike Carrickittle where high-grade mineralization is steeply
dipping, Ballywire mineralization appears to be bedding-parallel
along the base of the Waulsortian limestone. This implies
relatively enhanced tonnage potential, as well as,
similarities to the morphology of classic Irish-type zinc
deposits. Overall, with our compelling deep target at
Carrickittle West announced in June, high-grade massive
sulphides discovered nearby at Carrickittle in 2020 and
now this discovery at Ballywire, the prospectivity of our
extensive land package has never been more exciting. We look
forward to updating the market on next steps at
Ballywire and our other projects over the near term."
Regional Setting of the Ballywire
Zinc Prospect, PG West Project (100%-interest), Ireland
The Ballywire zinc prospect is located at the intersection of
the south-westerly projection of the Rathdowney Trend (which hosts
the historic Lisheen and Galmoy zinc mines) and the Pallas Green
Corridor (see Exhibit 1). Historic drilling at the prospect
was sparse, last being worked by operators in 2008. Group Eleven
staked the prospect in 2016 based on compelling results from the
two most-recent historic holes.
Notes to Exhibit 1: (a) Pallas Green MRE is owned by
Glencore (see Glencore's Resources and Reserves Report dated
December 31, 2021); (b) Stonepark
MRE: see the 'NI 43-101 Independent Report on the Zinc-Lead
Exploration Project at Stonepark, County
Limerick, Ireland', by Gordon, Kelly
and van Lente, with an effective date of April 26, 2018, as found on SEDAR; and (c) the
historic estimate at Denison was reported by Westland Exploration
Limited in 'Report on Prospecting Licence 464' by Dermot Hughes
dated May, 1988; the historic estimate at Gortdrum was reported in
'The Geology and Genesis of the Gortdrum Cu-Ag-Hg Orebody' by G.M.
Steed dated 1986; and the historic estimate at Tullacondra was
first reported by Munster Base Metals Ltd in 'Report on Mallow
Property' by David Wilbur, dated December 1973; and later
summarized in 'Cu-Ag Mineralization at Tullacondra, Mallow, Co.
Cork' by Wilbur and Carter in 1986; the above three historic
estimates have not been verified as current mineral resources; none
of the key assumptions, parameters and methods used to prepare the
historic estimates were reported and no resource categories were
used; significant data compilation, re-drilling and data
verification may be required by a Qualified Person before the
historic estimates can be verified and upgraded to be compliant
with current NI 43-101 standards; a Qualified Person has not done
sufficient work to classify them as a current mineral resource and
the Company is not treating the historic estimates as current
mineral resources. 'Rathdowney Trend' is the south-westerly
projection of the Rathdowney Trend, hosting the historic Lisheen
and Galmoy mines.
Drill Program at Ballywire, PG
West Project (100%-interest), Ireland
The 2022 drill program at Ballywire consisted of four step-out
holes totalling 1,400m (see
G11-468-02, G11-468-03, G11-2654-02 and G11-3552-01 in Exhibit
2). Individual holes stepped-out between 323-546m from G11-468-01, which intersected
3.30m of 12.5% Zn+Pb (10.1% Zn and
2.4% Pb) and 48 g/t Ag (see news release dated September 7th, 2021).
All four holes intercepted zinc mineralization; however,
G11-468-03 returned an especially wide interval containing many
high-grade lenses (see Exhibit 2, 3, 4 and 5). Also
noteworthy, a second hole, G11-3552-01 (a 546m step-out to the ESE from G11-468-01)
intersected a wide zone of mineralization over 38.55m grading 0.64% Zn+Pb (0.44% Zn and
0.20% Pb), including 0.58m of
4.54% Zn+Pb (3.25% Zn and 1.29% Pb) and 23 g/t Ag and
0.35m of 6.24% Zn+Pb (3.28% Zn
and 2.96% Pb) and 13 g/t Ag (see Exhibit 2 and 3).
High-grade mineralization consists of semi-massive and massive
sphalerite and galena, with lower grade zones consisting of
vein-hosted and/or disseminated sphalerite and galena (see
Exhibit 5).
Drilling to date at Ballywire consistently shows mineralized
zones to be generally bedding-parallel along the base of the
Waulsortian limestone (see Exhibit 3), similar to the
morphology of classic Irish-type zinc deposits. The base of the
Waulsortian limestone at Ballywire dips to the SSE, shallowing to
the NNW. Altogether, high-grade zinc-lead mineralization at
Ballywire is now pierced by three holes over approximately 1.5km
(see 97-468-02, G11-468-01 and G11-468-03 in Exhibit 2):
- 97-468-02 (1997): 2.50m of 6.21% Zn+Pb (3.00% Zn and 3.21% Pb),
including 0.50m of 20.28%
Zn+Pb (9.60% Zn + 10.68% Pb)
- G11-468-01 (2021): 3.30m of 12.48% Zn+Pb (10.11% Zn + 2.38% Pb)
and 48.3 g/t Ag, including 0.40m of 25.45% Zn+Pb (20.10% Zn and 5.35%
Pb) and 92.2 g/t Ag
- G11-468-03 (2022): 6.85m of 15.4% Zn+Pb (11.1% Zn and 4.3% Pb)
and 160 g/t Ag, including 2.05m of
40.8% Zn+Pb (30.5% Zn and 10.3% Pb) and 385 g/t Ag
The discovery area around G11-468-03 remains open and
untested along strike for approximately 3km to the ENE and
1.5km to the W, as well as, up-dip to the NNW for at least
500m (see Exhibit 2).
Notably, the next nearest historic hole testing the target horizon
to the ENE (99-3552-05) is 3km away and intersected 5.00m of 1.6% Zn+Pb. Immediate follow-up
drilling is highly warranted.
Assay results from G11-468-03 are summarized in Exhibit 4
and shown in full in in Exhibit 5.
Exhibit 4. Summary of Assays from G11-468-03 at Ballywire
Prospect, PG West Project, Ireland
Note
|
From
(m)
|
To
(m)
|
Interval
(m)
|
Zn
%
|
Pb
%
|
Zn+Pb
%
|
Ag
g/t
|
|
228.20
|
233.20
|
5.00
|
6.24
|
2.07
|
8.31
|
106.8
|
Including
|
228.20
|
230.23
|
2.03
|
13.94
|
4.89
|
18.83
|
227.7
|
|
|
|
|
|
|
|
|
|
251.65
|
258.50
|
6.85
|
11.06
|
4.34
|
15.40
|
160.3
|
Including
|
251.65
|
254.60
|
2.95
|
4.42
|
2.89
|
7.32
|
104.1
|
And
|
256.45
|
258.50
|
2.05
|
30.52
|
10.26
|
40.78
|
384.7
|
|
|
|
|
|
|
|
|
|
268.88
|
270.59
|
1.71
|
10.28
|
1.93
|
12.21
|
38.1
|
|
|
|
|
|
|
|
|
|
274.70
|
275.66
|
0.96
|
4.35
|
0.79
|
5.14
|
14.6
|
Note: True widths
estimated to be 80-100% of the downhole interval
|
Exhibit 5. Continuous Assays from G11-468-03 at Ballywire
Prospect, PG West Project, Ireland
From
(m)
|
To
(m)
|
Int
(m)
|
Zn
%
|
Pb
%
|
Zn+Pb
%
|
Ag
g/t
|
Lithology
|
222.04
|
225.09
|
3.05
|
0.89
|
0.32
|
1.21
|
8.3
|
WL w SPH in
veins
|
225.09
|
228.20
|
3.11
|
0.03
|
0.01
|
0.04
|
3.7
|
WL w PY
veins
|
228.20
|
228.57
|
0.37
|
21.40
|
3.76
|
25.16
|
171.0
|
MS pebbles - minor
cavity above
|
228.57
|
229.31
|
0.74
|
0.21
|
0.08
|
0.29
|
4.5
|
WL
|
229.31
|
229.87
|
0.56
|
32.70
|
13.70
|
46.40
|
632.0
|
MS lens SPH &
GAL
|
229.87
|
230.23
|
0.36
|
5.32
|
2.22
|
7.54
|
116.0
|
SPH + PY in
vein
|
230.23
|
230.80
|
0.57
|
1.37
|
0.47
|
1.84
|
68.4
|
WL - PY in
vein
|
230.80
|
231.45
|
0.65
|
0.93
|
0.18
|
1.10
|
17.6
|
WL - PY in
vein
|
231.45
|
232.41
|
0.96
|
0.55
|
0.06
|
0.61
|
11.0
|
WL - PY in
vein
|
232.41
|
233.20
|
0.79
|
1.23
|
0.02
|
1.25
|
13.4
|
WL - PY in
vein
|
233.20
|
248.87
|
15.67
|
0.15
|
0.06
|
0.21
|
3.6
|
WL w tr PY
|
248.87
|
251.65
|
2.78
|
0.38
|
0.06
|
0.44
|
24.3
|
WL/small dykes w semi-m
PY
|
251.65
|
252.82
|
1.17
|
5.35
|
1.09
|
6.44
|
106.0
|
MS - mainly PY w
GAL
|
252.82
|
253.82
|
1.00
|
3.54
|
4.56
|
8.10
|
113.0
|
MS - mainly PY + GAL +
SPH
|
253.82
|
254.60
|
0.78
|
4.17
|
3.47
|
7.64
|
89.7
|
MS - PY more SPH &
GAL
|
254.60
|
256.45
|
1.85
|
0.07
|
0.08
|
0.15
|
1.5
|
WL w tr PY
|
256.45
|
257.00
|
0.55
|
32.70
|
19.70
|
52.40
|
540.0
|
MS -
SPH/GAL/PY
|
257.00
|
257.81
|
0.81
|
32.10
|
10.40
|
42.50
|
339.0
|
MS -
SPH/GAL/PY
|
257.81
|
258.10
|
0.29
|
44.30
|
3.35
|
47.65
|
496.0
|
MS -
SPH/GAL/PY
|
258.10
|
258.50
|
0.40
|
14.35
|
2.00
|
16.35
|
183.0
|
MS -
SPH/GAL/PY
|
258.50
|
259.63
|
1.13
|
0.32
|
0.08
|
0.40
|
2.5
|
WL / BN contact, tr
SPH, PY
|
259.63
|
267.95
|
8.32
|
-
|
-
|
-
|
-
|
not yet sampled (low
grade)
|
267.95
|
268.88
|
0.93
|
0.28
|
0.03
|
0.31
|
1.6
|
BN w tr PY
|
268.88
|
269.72
|
0.84
|
17.35
|
1.99
|
19.34
|
55.2
|
BN - SPH cemented
BX
|
269.72
|
270.59
|
0.87
|
3.46
|
1.88
|
5.34
|
21.6
|
BN - SPH cemented
BX
|
270.59
|
273.10
|
2.51
|
0.31
|
0.10
|
0.41
|
2.0
|
BN
|
273.10
|
274.70
|
1.60
|
0.00
|
0.09
|
0.10
|
1.6
|
BN
|
274.70
|
274.95
|
0.25
|
4.44
|
1.12
|
5.56
|
13.4
|
BN - tr SPH in
fracture
|
274.95
|
275.66
|
0.71
|
4.32
|
0.67
|
4.99
|
15.0
|
BN - PY tuff on
shear
|
275.66
|
279.11
|
3.45
|
0.27
|
0.12
|
0.39
|
1.8
|
BN crackle BX w tr
SPH
|
279.11
|
287.37
|
8.26
|
-
|
-
|
-
|
-
|
not yet sampled (low
grade)
|
287.37
|
288.06
|
0.69
|
0.93
|
0.27
|
1.20
|
2.9
|
BST - SPH on small
fault
|
Note: shading above
denotes continuous zones of >1.0% Zn+Pb; "SPH" = sphalerite,
"GAL" = galena, "PY" = pyrite, "MS" = massive sulphide, "Semi-m" =
semi-massive sulphide, "WL" = Waulsortian Limestone, "BN" =
Ballynash Limestone; "BST" = Ballysteen Limestone; "BX" = Breccia,
"tr" = trace and "w" = with; unsampled intervals assumed to be nil
grade; true widths are estimated to be 80-100% of the downhole
interval; outside the above interval, trace zinc occurs first at
191.4m downhole and last at 297.1m downhole
|
Note that significant zinc-lead mineralization in G11-468-03,
occurs not only in the Waulsortian limestone, but also in the
sub-Waulsortian lithologies (i.e. Ballynash and Ballysteen
limestones; see Exhibit 5). This is not commonly observed in
Ireland outside of known zinc
deposits and may suggest the robust nature of the mineralizing
system and/or proximity to at least one of the feeder structures.
An example of high-grade mineralization from G11-468-03 is shown
below (see Exhibit 6).
Qualified Person
Technical information in this news release has been approved by
Professor Garth Earls, Eur Geol,
P.Geo, FSEG, geological consultant at IGS (International Geoscience
Services) Limited, and independent 'Qualified Person' as defined
under Canadian National Instrument 43-101.
Quality Assurance/Quality Control
(QA/QC) Information
Group Eleven inserts certified reference materials ("CRMs" or
"Standards") as well as blank material, to its sample stream as
part of its industry-standard QA/QC programme. The QC results have
been reviewed by the Qualified Person, who is satisfied that all
the results are within acceptable parameters. The Qualified Person
has validated the sampling and chain of custody protocols used by
Group Eleven.
About Group Eleven
Resources
Group Eleven Resources Corp. (TSX.V: ZNG; OTC: GRLVF and FRA:
3GE) is a mineral exploration company focused on advanced stage
zinc exploration in Ireland.
Additional information about the Company is available at
www.groupelevenresources.com.
ON BEHALF OF THE BOARD OF DIRECTORS
Bart Jaworski, P.Geo.
Chief Executive Officer
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.
Cautionary Note Regarding
Forward-Looking Information
This press release contains forward-looking statements within
the meaning of applicable securities legislation. Such statements
include, without limitation, statements regarding the future
results of operations, performance and achievements of the Company,
including the timing, content, cost and results of proposed work
programs, the discovery and delineation of mineral
deposits/resources/ reserves and geological interpretations.
Although the Company believes that such statements are reasonable,
it can give no assurance that such expectations will prove to be
correct. Forward-looking statements are typically identified by
words such as: believe, expect, anticipate, intend, estimate,
postulate and similar expressions, or are those, which, by their
nature, refer to future events. The Company cautions investors that
any forward-looking statements by the Company are not guarantees of
future results or performance, and that actual results may differ
materially from those in forward looking statements as a result of
various factors, including, but not limited to, variations in the
nature, quality and quantity of any mineral deposits that may be
located. All of the Company's public disclosure filings may be
accessed via www.sedar.com and readers are urged to review
these materials, including the technical reports filed with respect
to the Company's mineral properties.
SOURCE Group Eleven Resources Corp.