The western arm of the Lufilian Arc in NW Zambia and its potential for copper mineralization
Parts of the Kasai Shield, a western foreland to the Lufilian Arc and the western arm of this orogen are traced into NW Zambia. The Kasai Shield comprises a suite of metamorphic and igneous rocks (dated at ∼2540-2560 Ma) and extensive porphyritic granit
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|Source:||Journal of African Earth Sciences|
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