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Structural Mapping

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

Author(s): 
Bert De Waele and Jason Beltran
Category: 
CAD/GIS, Geology

Geological (Structural) mapping and data collection in the field form fundamental components of any effective exploration programme, regardless of commodity, mineralisation style or geological setting. The early adoption of effective mapping and field data collection strategies, from regional/ Read more... about The Digital Mapping Revolution: How to get the best of data capture in the field

Author(s): 
Bert De Waele, Mathieu Lacord, Fabio Vergara, Gavin Chan
Category: 
Geology
 
Three main types of iron mineralisation occur in West Africa: Palaeoproterozoic BIF-style on the Leo-Man Shield (e.g. Simandou), Neoproterozoic specularite of hydrothermal origin (e.g. in the Marampa Group), and metamorphic magnetite (e.g. in the Kasila Group). Understanding
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