Fathom Provides Gochager Lake Exploration Update

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Calgary, Alberta--(Newsfile Corp. - July 18, 2024) - Fathom Nickel Inc. (CSE: FNI) (FSE: 6Q5) (OTCQB: FNICF) (the "Company" or "Fathom") is pleased to provide the preliminary results from the field exploration program at the Company's 22,000+ ha Gochager Lake Property. The recently completed field program consisted of mapping, prospecting, detailed soil geochemistry analysis and detailed in-field core analysis.

Highlights of recent activity include:

  • Field crews mobilized to the project June 12th and completed field activities on June 30th.

    • Geological mapping, prospecting and soil geochemistry sampling was completed immediately over the historic Gochager Lake deposit area (see Figure 1).

    • From 2,047 soil sample locations, 1,757 B-horizon soils were collected, inclusive of QAQC duplicates.

    • Good outcrop exposure exists within the mapped area. This provided the opportunity to collect 50 outcrop samples that have been sent for whole rock and geochemical analysis.

    • Additionally, the good outcrop exposure allowed for the collection of 554 chip samples that were scanned using pXRF. The pXRF provides real-time geochemical data along with estimates of contained Ni-Cu-Co mineralization, as well as other key pathfinder elements.

      • Mineralization of up to 20,647ppm Ni (2.06% Ni), 6,922ppm Cu and 1,295ppm Co was noted in pXRF scans of outcrop material. *

    • The team identified zones of magmatic sulphide Ni occurring with coincident elevated Cr (chrome). Ni-tenors equal to and greater than those noted at the Gochager Lake deposit, occur to the north, southwest, and east of the deposit (see Figure 2).

    • Assay results for soils and rock samples are in early August.

  • Evaluation of geochemical results and reconciliation to drill core data is ongoing.

  • The Company has now reconciled the surface outcrop rock types with subsurface lithology defined to date by Fathom drilling. This exercise will continue to be very beneficial.

  • Unique mineral assemblages, recognized in drill core (specifically elevated Cr [chrome]), occurring in close association with mineralized, variable textured gabbro, have been detected in surface outcrops in proximity to the Gochager Lake deposit and further along strike (see Figure 2).

Ian Fraser, CEO and VP Exploration stated, "The recently completed and very productive field program at the Gochager Lake property has provided new, high-quality data to continue to demonstrate the presence of a significant magmatic Ni-Cu-Co deposit at Gochager. We are very excited to confirm that the same unique geochemical signals recognized in drill core is occurring in outcrop, 200-400 meters along strike. This is confirmation of a very open magmatic system. It is also very encouraging to now recognize the ultramafic rocks we encountered in drilling to depths in excess of 400 meters sub-surface are also occurring on surface and with significant Ni-tenor values. This suggests that the ultramafic rocks occurring within and proximal to the Gochager Lake deposit, if sufficiently saturated with sulphide, have the potential to host separate Ni-Cu-Co deposits. Our recent review of Mal Lake drill core is suggestive of this type of mineralization and confirmation that it is not just restricted to the historic Gochager Lake deposit area. The scale of potential at Gochager - both in the vicinity of the historic deposit, but also further afield, has now proven to be considerably larger than previously understood. This exercise will lead us into drill planning ahead of a proposed autumn drill program."