Regional Geology
The geology of the Asankrangwa Belt comprises strongly deformed Birimian meta-sediments, with minor granitic intrusions and mafic igneous rocks. The lithological units are cut by steeply north-west dipping primary and secondary structures. It is this combination of structural architecture and permissive lithologies that have been important in the localization of gold mineralization and provides the capacity for enhanced fluid flow forming major alteration systems associated with the gold bearing systems. The gold mineralization is linked to at least two separate deformation events and fluid emplacement, with many similarities to the gold deposits on the adjacent Sefwi and Ashanti Greenstone Belts.
Much of the Asankrangwa belt geological understanding and prospectivity mapping comes from a combination of airborne geophysical surveys such as VTEM and magnetics, and the wealth of accumulated geochemical and geological data. These datasets have allowed the company to develop our current pipeline of exploration targets.