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Hydrothermal alteration

Bert De Waele

The Mauritanide Belt occurs along the western margin of the West Africa Craton, and records a polyphase Neoproterozoic-Palaeozoic tectonothermal evolution spanning the period between 680 – 525 Ma.  The northern contact between the Mauritanide Belt and the West Africa Craton (Reguibat Shield) is Read more... about Structural control of hydrothermal alteration of BIF and formation of goethite-dominant mineralisation in the northern Mauritanide Belt

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