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The present work was carried out in the Matomb-Makak area located between meridians 11° and 11°15' East longitude and parallels 3°30' and 4° North latitude. At the junction between the Yaoundé series (in large part) and the Congo craton, this area appears to be a key sector for understanding the mapping of the Pan-African nappes north of the Congo craton. The lithological inventory highlighted six petrographic types: garnet and amphibole gneisses related to the Ntem complex (Congo craton) and Pan-African age formations including garnet chloritoschists, garnet amphibolites, garnet micaschists,…mehr

Produktbeschreibung
The present work was carried out in the Matomb-Makak area located between meridians 11° and 11°15' East longitude and parallels 3°30' and 4° North latitude. At the junction between the Yaoundé series (in large part) and the Congo craton, this area appears to be a key sector for understanding the mapping of the Pan-African nappes north of the Congo craton. The lithological inventory highlighted six petrographic types: garnet and amphibole gneisses related to the Ntem complex (Congo craton) and Pan-African age formations including garnet chloritoschists, garnet amphibolites, garnet micaschists, talcschists and garnet-distincter migmatites. Mineralogical assemblages show a multi-facial metamorphism with three main facies ranging from weak to strong: greenschists in the garnet chloritoschists (Chl+Qtz+Amph+Grt ±Pl) and talcschists (Tlc+Amph+Srp+Chl), upper amphibolites in the garnet and amphibole gneisses (Qtz+Grt+Pl+A
Autorenporträt
Nacido en 1977 en las tierras altas del oeste de Camerún, obtuve mi certificado de estudios primarios y mi bachillerato en Bamendjou, mi pueblo natal. En 1998, tras obtener el bachillerato, fui admitido en el primer año de la licenciatura de Ciencias de la Tierra en la Facultad de Ciencias de la Universidad de Yaundé I en Camerún.