DISTINCTION WITHIN THE CONGO CRATON IN SO UTH-WEST CAMEROON OF 2 DOLERITIC EPISODES INITIATING THE EBURNEAN (PALAEOPROTEROZOIC) AND PAN-AFRICAN (NEOPROTEROZOIC) OROGENIC CYCLES
Jp. Vicat et al., DISTINCTION WITHIN THE CONGO CRATON IN SO UTH-WEST CAMEROON OF 2 DOLERITIC EPISODES INITIATING THE EBURNEAN (PALAEOPROTEROZOIC) AND PAN-AFRICAN (NEOPROTEROZOIC) OROGENIC CYCLES, Comptes rendus de l'Academie des sciences. Serie II. Sciences de la terre et des planetes, 323(7), 1996, pp. 575-582
The dolerites which crosscut the Congo craton in South-West Cameroon b
elong to two distinct episodes of pre-orogenic extensions. The first e
pisode, ante-Eburnean, displays the geochemical characteristics of bac
k-are basin tholeiites and of greenstone belt volcanics, and is linked
to the opening of the Nyong Palaeoproterozoic basin. The second episo
de, ante-Pan-African, has the composition of typical continental thole
iites and is related to the formation of the Yaounde Neoproterozoic ba
sin.