To serve you better, our new website displays information specific to your location.
Please visit the site and bookmark it for future use.

New SRK Global website

Hydrothermal alteration

Structural control of hydrothermal alteration of BIF and formation of goethite-dominant mineralisation in the northern Mauritanide Belt

Author(s):

Bert De Waele

Category:

Geology

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