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lepidolite |
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London and Evensen, 2002); (3) an increase in the Ca content of the fluids by interaction with the host schist; (4) an increase in host-rock permeability or porosity reflecting either rock type differences or fracture propagation related to deformation accommodating cooling of the granite pluton below; (5) precipitation of lepidolite within the vein selvage, removing F (ligand) and Li (buffer) from the fluids; or (6) simply because of decreases in pressure and/or temperature. Minerals occurring in association with the tantalite include; spodumene, beryl, tourmaline, lepidolite and muscovite. These holes were drilled on the eastern and western extensions of the Big Whopper system and on a newly-outlined dyke enriched in the lithium-rubidium mineral lepidolite ("the Lepidolite Dyke"), that is situated immediately northeast of the Big Whopper. |
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