Cambro-Ordovician palaeogeography and fragmentation of the North Gondwana margin is still not very well understood. Here we address this question using isotopic data to consider …
J Penaye, SF Toteu, R Tchameni… - Journal of African Earth …, 2004 - Elsevier
Available isotopic and geochronological data, combined with new petrographic and structural observations in Cameroon, permit discussion of the nature and extension of the …
E Ferré, G Gleizes, R Caby - Precambrian research, 2002 - Elsevier
The Eastern Nigeria terrane belongs to the 3000 km-long Trans-Saharan belt which was formed in the Neoproterozoic, between 750 and 500 Ma by continental collision between the …
EC Ferré, R Caby, JJ Peucat, R Capdevila, P Monié - Lithos, 1998 - Elsevier
Three Pan-African hypersthene-bearing monzogranitic and quartz–monzonitic plutons from the Eastern terrane of Nigeria have been investigated in detail. New major, trace and REE …
T Njanko, A Nédélec, M Kwékam, R Siqueira… - Journal of Structural …, 2010 - Elsevier
The Fomopéa pluton (622–613 Ma) is located in the western part of the Pan-African belt in Cameroon. It comprises of 3 units: biotite-hornblende granitoids (BHG), biotite …
G Njiekak, W Dörr, JP Tchouankoué, G Zulauf - Lithos, 2008 - Elsevier
Striking characteristics of the western Neoproterozoic belt of Cameroon (NFBC) are the large volume of granitoids and crustal-scale shear zones. New structural and …
P Affaton, A Kröner, KF Seddoh - International Journal of Earth Sciences, 2000 - Springer
Metamorphic zircons from seven granulite facies orthogneisses of tonalitic composition (enderbites), collected from four different nappes of the Kabye Massif in the Dahomeyide …
M Kwékam, I Dunkl, EM Fozing, G Hartmann, T Njanko… - 2021 - pubs.geoscienceworld.org
Abstract The Dschang granites, SW Cameroon, are post-Panafrican granitoids, hosted in Paleoproterozoic orthogneiss in the Western domain of the Central African fold belt. They …
MJ De Wit, S Bowring, R Buchwaldt… - South African Journal …, 2021 - journals.co.za
In 1964, WQ Kennedy suggested that the crust of Saharan Africa is different from the rest of Africa. To date, the geologic evolution of this region remains obscure because the age and …