DISTINCTION WITHIN THE CONGO CRATON IN SO UTH-WEST CAMEROON OF 2 DOLERITIC EPISODES INITIATING THE EBURNEAN (PALAEOPROTEROZOIC) AND PAN-AFRICAN (NEOPROTEROZOIC) OROGENIC CYCLES

Citation
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
Citations number
28
Categorie Soggetti
Geosciences, Interdisciplinary
ISSN journal
12518050
Volume
323
Issue
7
Year of publication
1996
Pages
575 - 582
Database
ISI
SICI code
1251-8050(1996)323:7<575:DWTCCI>2.0.ZU;2-V
Abstract
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.