Historic Drill Logs Reveals Pegmatites Intersected in Multiple Drill Holes at Big Bang Lithium Project

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TORONTO, ON / ACCESSWIRE / February 15, 2023 / High Tide Resources Corp. ("High Tide" or the "Company") (CSE:HTRC) is pleased to report that it has observed pegmatite in the historic drill logs of the Big Bang Lithium Project ("Big Bang" or the "Property"). Pegmatites are typically an important source of valuable lithium ore such as spodumene. It was revealed that notable widths of pegmatite were intersected in three holes drilled in 1968. The Property is located approximately 70 km east of Rock Tech Lithium's advanced-stage Georgia Lake property and 275 km northeast of Thunder Bay, Ontario near the town of Geraldton (Figures 1, 2 & 3).

Report "DD RPT 10 GAMSBY LAKE" found within Ontario Assessment File 42E11SW0101 indicates that all three diamond drill holes (total footage 545 ft or 166 m) drilled in July & August of 1968 by Chimo Option intersected pegmatite. At the time, Chimo Option was targeting the pegmatite zones for uranium and only assayed for U3O8 with results in the nil to trace range. Of particular interest is hole H1 that was drilled N55E at -45 degrees to a length of 362 feet (110 m) with approximately 58% of the core being logged as pegmatite. Pegmatite intercepts ranged from <1 m to plus 20 metres with the final 24 metres logged as, and ending in, pegmatite (Figures 4, 5 & 6). The whereabouts of the drill core is currently unknown.

Steve Roebuck, Director, President & Interim CEO of High Tide states, "Big Bang is a very exciting property with pegmatites having been mapped on surface and intersected in three drill holes. The 1968 drill program was focused on assessing the uranium potential of the pegmatite with no attention paid to the lithium potential. The 55-year-old drill logs are vague and contain no details about the mineralogical composition of the pegmatite but the macro geological and structural conditions, in and around the property, create favourable conditions for lithium bearing minerals to be present. High Tide will conduct a site visit in the spring to assess the area and prepare for a summer exploration program."

The property is underlain by a muscovite-bearing, S-type, peraluminous, fertile granite intruding metasediments (Figure 7). The Property occurs within 3 km of a subprovince boundary, and the Long Lac Fault and secondary structures provide excellent pathways for granitic melts and pegmatite deposition (Figure 8). Mapping in the Big Bang area in 1939 identified several instances of ‘granite' pegmatite (Figure 9). However, mapping during this era did not recognize, or document, various other ‘types' of pegmatites which contain important mineralogical information.