VANCOUVER, BC, Feb. 2, 2022 /CNW/ - Group Eleven Resources Corp.
(TSXV: ZNG) (OTC: GRLVF) (FRA: 3GE) ("Group Eleven" or
the "Company") is pleased to announce that drilling has
started on its Stonepark project ("Stonepark", 76.56% Group
Eleven, 23.44% Arkle Resources PLC), Ireland. Separately, plans for the Company's
initial drilling at the recently staked Tullacondra Copper-Silver
Prospect ("Tullacondra"), near the PG West Project ("PG
West"), are also underway.
Highlights:
- First hole of a six-hole program at Stonepark (totalling
2,300m; see news release dated
January 19, 2022) began yesterday at
the Carrickittle North locality
- With a target depth of 750m, this
hole represents a 250m step-out from
previous drilling, targeting the unexplored southern margin of the
Limerick Volcanic Complex, which management believes has the
potential to host zinc mineralization similar to Glencore's nearby
Pallas Green zinc-lead deposit1
- Separately, at Tullacondra, the Company is finalizing plans to
drill one hole (approx. 150m depth),
starting in the next 4-8 weeks
- Tullacondra hosts a historic estimate2 of
copper and silver (from 1973) and, from regional drilling in 2012
by a previous operator, also appears to contain elevated cobalt
levels (based on XRF data, which have yet to be confirmed and
followed-up)
- Historic core from Tullacondra cannot be located (assumed lost
and/or discarded) and historic data is quite limited (containing
only four elements: Cu, Ag, Zn, Pb)
- Hence, the aim of Tullacondra drilling will be to ascertain how
mineralization at the prospect compares to Group Eleven's other
Cu-Ag prospects (Gortdrum, Denison and Oola) and try to determine
if the prospect has potential for economic cobalt
mineralization
- Above work will help determine how Tullacondra ranks versus
other prospects in terms of exploration potential and may offer
insights into ongoing exploration at the Stonepark and PG West
projects
"We are excited to begin our drill hole at Carrickittle North,
targeting similar structure and geology to Glencore's Pallas Green
zinc deposit, located less than 10 kilometres along trend to the
north. We also very much look forward to conducting our
long-awaited drilling at Tullacondra," stated Bart Jaworski, CEO. "With strong, near-surface
copper-silver mineralization over hundreds of metres of strike,
Tullacondra has been in our sights for a long time. Aside from
trying to find look-alike zones of mineralization in the
neighbourhood, it is equally intriguing that the prospect's
potential for cobalt has never been advanced and yet, may provide a
brand-new avenue for exploration on the property."
Background Information on the Tullacondra Prospect at the PG
West Project (100%-interest), Ireland
The Tullacondra prospect is located approximately 20km south of
the Company's PG West project (see Exhibit 1). Group Eleven
applied for the Tullacondra property in early 2020 and was granted
the prospecting licenses in Sept
2020. The prospect shares similarities to Group Eleven's
Gortdrum, Denison and Oola Cu-Ag prospects, especially given that
mineralization appears to be related to volcanics. Located 1km to
the east of the Tullacondra historic estimate, for example, an
exposure of pyroclastic volcanic material (see
Exhibit 2) is believed to represent a larger volcanic
vent breccia, with the age of volcanism believed to be
similar to that at Group Eleven's Stonepark and PG West
projects.
Tullacondra hosts two adjacent and distinct historic estimates:
(a) 3.6 million tonnes of 0.7% copper and 27 g/t
silver ("copper-rich zone"); and (b) 0.6 million tonnes
of 150 g/t silver and 0.6% copper ("silver-rich zone"; see
Exhibits 2 and 3). The historic estimates at Tullacondra
were first reported by Munster Base Metals Ltd. in 1973 and later
summarized by Wilbur and Carter in 1985; the 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.
The copper-rich zone occurs as a
near-vertical body (see Exhibit 3) approximately
25-40m thick, extending from
near-surface to a vertical depth of at least 120m and extending for a strike length of
370m in an E-W orientation.
Mineralization is composed predominantly of bornite and
chalcopyrite (occurring as small veins, disseminations and blebs)
and mostly hosted in carbonate (limestone) lithologies above the
Old Red Sandstone (albeit, some mineralization appears to also
occur deeper in the stratigraphy).
The silver-rich zone occurs as a gently-dipping,
strata-bound horizon (see Exhibit 3; approximately
5-10m thick, 300m strike length, 250m dip extent), occurring at the base of the
copper-rich body. Mineralization consists predominantly of
tennantite-tetrahedrite and native silver (highest grade attained
historically was 426 g/t Ag over 1.5m). The silver-rich horizon occurs along a
distinctive hematite-bearing (iron oxide rich) marker
horizon. This horizon is about 30cm thick, albeit varies in
thickness, and is observed throughout the property.
In 2012, a previous operator focussing on Cu-Ag exploration,
drilled five regional holes within several kilometres of the
historic estimate, intersecting the hematite horizon within three
of the holes (the two others were abandoned prior to reaching the
hematite horizon). XRF analysis was conducted on portions of each
hole (X-ray fluorescence is a quicker and less expensive
alternative to traditional laboratory assay).
Two of these holes returned strongly elevated
cobalt levels. 'AM08' returned a 6.5m zone (starting at a downhole depth of
15.0m) with consistently elevated
cobalt readings generally ranging between 100-510 ppm, with a high
of 1434 ppm Co; whereas, 'AM09' returned much spottier
readings, albeit, containing two strong kicks of 1,086 ppm
Co and 8,102 ppm Co at a depth of 18.00m and 19.5m,
respectively3. Given the XRF program was quite limited
(restricted to the first several metres of each hole), the above
readings were inadvertently collected proximal to the hematite
horizon, but not at the hematite horizon itself.
Given the low prices at the time, cobalt was not a focus.
Similarly, the Tullacondra historic estimate has never been
analysed for cobalt (historic assays consist only of Cu, Ag, Zn and
Pb). Further work is required to determine the nature and extent of
cobalt mineralization on the property and to determine if such
mineralization might be present at the historic estimate, within
the hematite-layer and/or potentially elsewhere on the
property.
Notes to Exhibit 1: (a) Pallas Green MRE is owned by
Glencore; (b) Stonepark MRE: please refer to the NI 43-101
Independent Report on the Zinc-Lead Exploration Project at
Stonepark, County Limerick,
Ireland, with an effective date of April 26, 2018, as found on SEDAR; (c) the
historic estimate at Denison was reported by Westland Exploration
Limited in 1988, the historic estimate at Tullacondra was reported
by Munster Base Metals Ltd in 1973 and the historic estimate at
Gortdrum was reported by G.M. Steed in 1986; these 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.
Note: Modified from
Diversified Asset Holdings (2016)
|
_______________
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1
Resources and Reserves Report (Glencore, December 31, 2020) – 45.4
million tonnes of 7% Zn + 1% Pb (Inferred)
|
2 3.6mt of
0.7% Cu and 27 g/t Ag and 0.6mt of 150 g/t Ag and 0.6% Cu (Source:
Munster Base Metals Ltd., 1973; Wilbur and Carter, 1985)
|
3 Report
by Mayfly Resources Ltd. (dated 20 May 2013) – XRF readings were
taken every 5cm and averaged for each 50cm
interval;
|
Qualified Person
Technical information in this news release has been approved by
Paul Gordon, P.Geo., geological
consultant at SLR Consulting, and independent 'Qualified Person' as
defined under Canadian National Instrument 43-101.
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.
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.