MONTREAL, QC / ACCESSWIRE / February 13, 2024 / SRQ Resources Inc. (TSX-V:SRQ) ("SRQ" or the "Company") is pleased to announce it has further characterised the nickel and copper mineralisation of Lac Brulé's recently discovered Ultramafic Magmatic ("UM") intrusive complex using petrological and mineralogical studies of samples.

Dr. Marc-Antoine Audet, SRQ's President & CEO, will present the findings and the 2024 projected exploration program during a live virtual non-deal roadshow hosted by Renmark Financial on Wednesday, February 14, 2024, at 12:00 P.M. EST. Investors and interested parties are invited to register here using the latest version of Google Chrome. Access to a replay of the event will be available on the SRQ website or on Renmark Financial's website at www.renmarkfinancial.com/vndrs.

Highlights of Mineralisation Characteristics at Lac Brulé's UM Complex:

UM complex is composed of meta-pyroxenite and meta-peridotite, both of which intrude the highly metamorphic host rock sequence:
The meta-pyroxenite includes locally porphyritic assemblages of diopside, magnesio-hornblende and olivine (Fo80-84) with a lesser proportion of enstatite, intercalated with mineralized horizons containing up to 30% sulphides
Sulphides present are mainly pyrrhotite (iron + minor nickel ("Ni")), chalcopyrite (copper ("Cu")); cobalt-rich pentlandite (Ni and cobalt ("Co"))
Lower than expected nickel was observed in the olivines in the meta-peridotite, suggesting their transfer to the sulphide's liquids during immiscibility

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