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A recent airborne geophysics survey confirmed a strong east-west magnetic anomaly coincident with historical surface mapping of pegmatites over an area 9 kilometres long and up to 700 metres wide. The host intermediate/mafic magnetic rocks confirmed through the survey have been intruded by discrete outcrops of sub-parallel lithium, beryllium, and tantalum-bearing, granitic pegmatite dykes. The conjunction of east-west trending pegmatite dykes dipping to the north and hosted by metamorphic ultramafic and schist rocks is a similar geological setting observed at Authier.
Ann: High-Grade Lithium Assays Returned From Tansim Sampling, page-6
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