OTTAWA,
ON, Oct. 17, 2023 /CNW/ - Northern Shield
Resources Inc. ("Northern Shield" or the "Company") (TSXV:
NRN) is pleased to announce that the diamond drilling program
at the Root & Cellar Gold Project (the "Project"), located on
the Burin Peninsula in
southeastern Newfoundland, has
been completed, with visible gold noted in three of the eight drill
holes (Table 1). The Company can earn a 100% interest in the
Project, which is being explored for epithermal gold-silver and
porphyry-copper type mineralization, both with associated tellurium
(Te).
Eight drill holes (23RC-15 to 22), totalling 615 metres,
were completed (Figure 1) with 200 drill core samples taken for
analysis. The drilling program tested shallow IP geophysical
anomalies in the vicinity of surface mineralization in the Conquest
Zone. Seven of the eight drill holes intersected
quartz/silica-pyrite +/- clay breccias and associated argillic to
propylitic alteration consistent with a low-sulphidation,
epithermal, gold system. Five occurrences of visible gold were
noted in drill holes 23RC-16, 18 and 21 (Figure 2). Mineralized
zones show multiple phases and styles of brecciation (Figure 3) and
replacement textures with common, abundant pyrite (and/or
marcasite) in silica and locally clay rich matrixes. What are
interpreted to be hydrothermal mill breccias, (including the
"Oatmeal Breccia") are a common phase in the Conquest Zone, and
host two of the visible gold occurrences in drill core (Figure
4).
Much of the mineralization intersected is hosted in andesitic
lapilli tuffs and adjacent rhyolite spires, and associated carapace
breccias. It appears that the porosity of the tuffs and voids in
breccia units acted as a sponge for the initial hydrothermal fluids
prior to repeated brecciation events, each event bringing in more
clay minerals, silica and pyrite.
The mineralization in drill core, along with the corresponding
IP chargeability anomalies, fall on the edge of, or within, a zone
of low resistivity. Clay minerals, ubiquitous in epithermal systems
as alteration products, along with the observed stringer pyrite,
could create these resistivity lows which, with the IP
chargeability anomalies that coincide with its margin, provide an
extensive target area.
Future drilling will test the mineralized intervals laterally,
and to depth, along the margin of the geophysical anomalies.
"We are very happy with what we see in core from this small
drilling program. Not only have we intersected multiple intervals
of promising looking mineralization and visible gold within 40
metres of surface, we have also gained valuable knowledge of the
geology and the likely causes of the geophysical signatures, and a
refined understanding of the epithermal system. The multiple phases
of hydrothermal brecciation, of which most, if not all carry
pyrite, is a good sign as every progressive hydrothermal event
provides the opportunity to increase gold grades and grow the
epithermal system. Although we need to wait for assay results, we
are very pleased with the results from the completed drilling
program and we are optimistic about future drilling programs
targeting the Conquest Zone".
- Ian Bliss,
Northern Shield President and CEO
Table 1. Summary of significant drill core intervals.
23RC-15
|
2.5 metres of
hydrothermal breccias and alteration consisting of grey amorphous
quartz vein and quartz vein fragments with disseminated pyrite in
silica-pyrite rich matrix and a further 4.5 metres of mixed
breccias and intense alteration with pyrite.
|
23RC-16
|
4.9 metres of crackle
breccia consisting off-white siliceous fragments with chlorite
fractures, patches of very fine-grained pyrite and disseminated
pyrite associated with second phase of silicification. Some coarser
pyrite with translucent quartz blebs and veinlets. Some stringer
pyrite
4.9 metres of dominated
by translucent quartz blebs and quartz vein fragments with
disseminated pyrite and bladed marcasite Visible gold noted.
2 zones totalling 6
metres of hydrothermal breccia including "Oatmeal Breccia", and
rounded quartz blebs in a silica-pyrite matrix. Visible gold
noted.
3 metre interval
containing 5% quartz-hematite veins with minor pyrite.
|
23RC-17
|
1.6 metres of patches
of grey silica and white quartz veins and blebs with fine
pyrite.
11.5 metres of
hydrothermal breccia and mineralized carapace breccia consisting
mostly of grey quartz vein and quartz vein fragments, some creamy
silica (adularia?) fragments, all with disseminated pyrite, minor
bladed marcasite and patches of fine-grained pyrite.
3.4 metres of
hydrothermal mill breccia including "Oatmeal Breccia" consisting
mostly of rounded quartz fragments in silica-pyrite matrix and
minor marcasite.
|
23RC-18
|
2.3 metres of
hydrothermal mill breccia including "Oatmeal Breccia" consisting
mostly of brecciated amorphous quartz and fragments of bluish-grey,
crustiform silica and an indigo blue quartz with significant
pyrite. Visible gold noted.
A further 3.3 metres
of moderate silicification and pyrite.
|
23RC-19
|
No significant
noteworthy mineralization noted.
|
23RC-20
|
4.8 metres of
hydrothermal breccia and mineralized carapace breccia consisting
mostly of very fine disseminated
pyrite throughout siliceous matrix and local coarser pyrite along
the margins of white quartz veinlets and blebs.
|
23RC-21
|
Visible gold in
quartz veinlet with relatively little wall rock alteration.
2.3 metres of
hydrothermal brecciation and alteration with the development of
creamy white silica (adularia?) with some quartz veinlets,
disseminated and stringer e.
1 metre of dominantly
creamy beige brecciated quartz-adularia? with stringer pyrite
veinlets, white translucent quartz veinlets with and without
pyrite.
2.4 metres of smoky
grey, banded and brecciated amorphous silica with extremely
fine-grained pyrite and pyrite stringers; some remnants of creamy
silica-adularia veins/fragments.
Several zones totalling
2.5 metres of dark grey, brecciated cryptocrystalline quartz and
milled quartz breccia (oatmeal breccia) with some pink adularia?
coming in with silica.
|
23RC-22
|
Two zones totalling 2
metres of greyish-white quartz breccia with matrix of bluish white
silica/sericite and pyrite with fragments of white
quartz.
|
The drilling project along with this news release was overseen
by Christine Vaillancourt, P. Geo.,
the Company's Chief Geologist and a Qualified Person under National
Instrument 43-101.
About Northern Shield
Northern Shield Resources Inc. is a Canadian-based company,
known as a leader in generating high-quality exploration targets,
that views greenfield exploration as an opportunity to
discover a near surface, tier one asset, at relatively low cost. We
implement a model driven approach in exploration to reduce risks
associated with early-stage projects for ourselves, our
shareholders, and the environment. This approach is what led to the
discovery of an alkaline-related gold-silver-tellurium and porphyry
copper system at the Root & Cellar Project in Newfoundland.
Forward-Looking Statements Advisory
This news release contains statements concerning the
exploration plans, results and potential for epithermal gold
deposits, and other mineralization at the Company's Root &
Cellar Property , geological, geophysical and geometrical analyses
of the properties and comparisons of the properties to known
epithermal gold deposits and other expectations, plans, goals,
objectives, assumptions, information or statements about future,
conditions, results of exploration or performance that may
constitute forward-looking statements or information under
applicable securities legislation. Such forward-looking
statements or information are based on a number of assumptions,
which may prove to be incorrect.
Although Northern Shield believes that the expectations
reflected in such forward-looking statements or information are
reasonable, undue reliance should not be placed on forward‑looking
statements because Northern Shield can give no assurance that such
expectations will prove to be correct. Forward-looking
statements or information are based on current expectations,
estimates and projections that involve a number of risks and
uncertainties which could cause actual results to differ materially
from those anticipated by Northern Shield and described in the
forward‑looking statements or information. These risks and
uncertainties include, but are not limited to, risks
associated with geological, geometrical and
geophysical interpretation and analysis, the ability of
Northern Shield to obtain financing, equipment, supplies and
qualified personnel necessary to carry on exploration and the
general risks and uncertainties involved in mineral exploration and
analysis.
The forward-looking statements or information contained in this
news release are made as of the date hereof and Northern Shield
undertakes no obligation to update publicly or revise any
forward‑looking statements or information, whether as a result of
new information, future events or otherwise, unless so required by
applicable securities laws.
Neither TSX Venture Exchange nor its Regulation Services
Provider (as that term is defined in policies of the TSX
Venture Exchange) accepts responsibility for the adequacy or
accuracy of this release.
SOURCE Northern Shield Resources Inc.