Churchill Identifies Mineralized Magmatic Intrusive System at Taylor Brook Ni-Cu Project, Western Newfoundland
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Churchill Identifies Mineralized Magmatic Intrusive System at Taylor
Brook Ni-Cu Project, Western Newfoundland
TORONTO, November 18, 2021 (GLOBE NEWSWIRE) – Churchill Resources Inc. (“Churchill”
or the “Company”) (TSXV: CRI) is pleased to announce that its Phase 1 Exploration Program at
Taylor Brook in western Newfoundland has proceeded well and has identified and started to
evaluate a magmatic Ni-Cu system on the property which appears to have significant scale.
• Historic drilling of the Layden Showing in 2008 returned 4.25 m of 1.63% Ni, 0.36% Cu
and 0.027% Co in hole 08-TB-17
• Recent Churchill drilling and mapping indicate that Layden may be part of a much larger
mineralized magmatic system of sulphide breccia structures within a gabbroic intrusive
• Sulphide-cemented breccia structures have been intersected in several locations over
~100m along the overall gabbroic intrusive thus far, at depths from surface to ~-200m.
• mineralized breccia structures appear to range from 5-15m wide with sulphide contents
up to 40% (pyrrotite-pendlandite-chalcopyrite) locally over 10-20cm
• Assay results are expected from Churchill’s 2,477m Phase 1 drilling program towards the
end of the year
Paul Sobie, Chief Executive Officer of Churchill remarked, “We are really excited by the drilling
and surface mineralization at Taylor Brook, which indicate that we are intersecting lithologies and
textures related to magmatic Ni -Cu deposits. We look forward to continuing to evaluate this
magmatic system and potentially locating more massive styles of mineralization, as well as any
other systems we may discover on the overall property.”
Taylor Brook Project
To date 13 core holes totalling 2,477m have been drilled as the Phase 1 program, of which several
holes were positioned geologically to define the emerging magmatic system. Others were
targeted on VTEM conductor plates, all of which have helped to establish a preliminary model for
this portion of the overall property, as per the figure below which shows current and historical
drilling over unprocessed recently collected total field ground magnetics.
Drilling, mapping and geophysical surveys indicate that the mineralized outcrop at the original
Layden Showing appears to be part of a much larger intrusive magmatic Ni -Cu system striking
east-southeast and plunging to the southeast with significant thickness es based on drill
intersections. The Layden magmatic system is hosted by a discrete, magnetic, meta-gabbroic to
meta-pyroxenitic intrusion within basement gneisses with the Ni-Cu mineralization taking the form
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of pods, thin horizons and blebs of pyrrhotite, pentlandite and chalcopyrite that brecciate the
pyroxenite.
The sulphide-cemented breccia structures have been intersected in several locations over ~100m
along the overall gabbroic intrusive at depths from surface to ~-200m. The mineralized breccia
structures appear to range from 5-15m wide with sulphide contents up to 40% locally over 10-
20cm with several separate zones of breccia within the Layden intrusion.
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Bore Hole Electromagnetic (BHEM) surveys on all holes are being conducted to assist in planning
deeper Phase 2 drilling. Logging and sampling of Phase 1 holes is nearing completion as well, a
large suite of samples has been selected for geochemical analysis, petrography and in some
cases, radiometric age dating to aid in understanding the host and intrusive rocks and
mineralization event.
A heavy minerals sampling program along the western margin of the very large Taylor Brook
Gabbro Complex which outcrops less than a kilometre east of the mineralized magmatic intrusive
at Layden is currently underway. Drilling results are expected toward the end of 2021.
Florence Lake Project
A helicopter-borne VTEM and Horizontal Gradiometer Geophysical Survey is commencing at the
Florence Lake Project in Labrador.
The Florence Lake Property contains Raglan-type ultramafic volcanic -hosted massive and
disseminated sulphide nickel showings, and was last explored by Falconbridge and JV partners
between 1990-1997 during which time approximately 6,250m of drilling was completed in 45
shallow holes . 1996 drill core is located on the property for relogging and sampling, whereas
1992-3, partly sampled core, is stored at NL Government core library in Happy Valley – Goose
Bay. Highlights of that work included drill testing of the high-grade Baikie Showing where shallow
drilling (<-100m depths) returned:
DDH FLK-92-02: 2.19% Ni, 0.22% Cu, 0.16% Co over 11.32 metres from 44.7 to 56m
DDH FLK-92-12: 1.33% Ni, 0.05% Cu over 13.5 metres from 83.0 to 96.5m
The Baikie Showing has demonstrated mineralized continuity over 110m of strike length from
twelve drillhole intercepts and mapping, and is interpreted as a near vertically plunging subzone
of disseminated, semi -massive and massive sulphide mineralization, possibly similar to the
Raglan or Kambalda style of nickel deposits. Other showings along strike have generated +1.0%
nickel grab samples or short drill intersections and need modern exploration work along with
Baikie.
Churchill announced positive results of due-diligence resampling of the historical core in a news
release dated October 7, 2021.
The technical and scientific information in this news release has been reviewed and approved by
Dr. Derek H.C Wilton, P.Geo., FGC, who is a “qualified person” as defined under National
Instrument 43-101 – Standards of Disclosure for Mineral Projects and independent of the
Company. The Churchill drill core samples are half core samples laid out and split by qualified
geologists and technicians under the direction of Senior Project Consultant Dawn Evans -
Lamswood, P.Geo. at the Company’s drill camp near the property. The samples were placed in
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labelled, sealed plastic bags and periodically batches are delivered to Eastern Analytical for
analysis. Standard OREAS 13b and blanks were inserted in the assay batches.
About Churchill Resources Inc.
Churchill is managed by career mining industry professionals and currently holds four exploration
projects, namely Taylor Brook in Newfoundland, Florence Lake in Labrador, Pelly Bay in Nunavut
and White River in Ontario. All projects are at the evaluation stage, with known mineralized Ni-Cu-
Co showings at Taylor Brook, Florence Lake and Pelly Bay, and diamondiferous kimberlitic intrusives
at White River and Pelly Bay. The primary focus of Churchill is on the continued exploration and
development of the Taylor Brook and Florence Lake Nickel Projects.
Further Information
For further information regarding Churchill, please contact:
Churchill Resources Inc.
Paul Sobie, Chief Executive Officer
Tel. +1 416.365.0930 (o)
+1 647.988.0930 (m)
Email [email protected]
Alec Rowlands, Corporate Consultant
Tel. +1 416.721.4732 (m)
Email [email protected]
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