Unlock stock picks and a broker-level newsfeed that powers Wall Street.

G2 Files Independent Technical Report; Provides Greenfields Exploration Update

In This Article:

G2 Goldfields Inc.
G2 Goldfields Inc.

TORONTO, Jan. 14, 2025 (GLOBE NEWSWIRE) -- G2 Goldfields Inc. (“G2” or the “Company”) (TSX: GTWO; OTCQX: GUYGF) announces the filing of an independent technical report dated December 13, 2024, on the Company’s newly acquired 32,906-acre New Aremu Project, Guyana. The Report, ‘NI 43-101 Property of Merit Technical Report for the New Aremu Oko Gold Project, Guyana, South America’, is available on SEDAR+ (www.sedarplus.ca). Additionally, G2 is pleased to provide an update on the Company’s ongoing greenfields exploration program across the entire exploration portfolio.

G2 intends to spin-out its interest in certain greenfields, non-core assets, into a wholly owned subsidiary of G2, G3 Goldfields Inc. (G3), through a plan of arrangement under the Canada Business Corporations Act [see press release dated January 06, 2025].

Following the completion of the proposed Spin-out, the exploration assets to be held by G3 include:

  • the New Aremu Project (including the historic Wariri Mine), Cuyuni District, Guyana (32,340 acres);

  • the Aremu Mine Property, Cuyuni District, Guyana (8,811 acres);

  • the Amsterdam Option, Cuyuni District, Guyana (7,148 acres);

  • the Tiger Creek Option, Puruni District, Guyana (3,685 acres); and

  • The Peters Mine Property, Puruni District, Guyana (8,316 acres).

It is anticipated that additional gold assets will be acquired for the G3 portfolio.

Technical Report

The independent Technical Report describes geology of the New Aremu project as follows:

“… The bedrock in the region is underlain by metavolcanics and metasediments of the late Proterozoic Cuyuni Formation, including sandstones, conglomerates and volcanics, intruded by several granitoid plutons. The Lower Aremu and East Aremu properties are bounded by the Aremu batholith to the west and the Bartica intrusive complex to the east. The Upper Aremu properties are bounded by the Aremu Batholith to the east.”

The Report notes gold mineralization in in-situ quartz veins and boulder trains in two areas.

“Large boulders of quartz interpreted as floats from nearby quartz reefs have been confirmed on both the Upper Aremu and Lower Aremu groups of properties. At the Upper Aremu properties quartz boulders up to 5 metres in diameter were observed as sub-crops along a 100-metre trend. The quartz boulders had a distinct laminated texture and were trending in a general north – south direction parallel to a nearby in-situ vein within a felsic intrusive saprolite that is likely the Aremu batholith.”

Table 7.1
Table 7.1


“Additionally, from a third area at the Aremu East group of properties a quartz vein varying between 5 cm to 40 cm hosted by the Aremu batholith was investigated (Figure 7.12). Two grab samples taken on this structure assayed 9.9 g/t Au and 18.5 g/t Au.”