Article citationsMore>>
E. Jagoutz, H. Palme, H. Baddenhaussen, K. Blum, M. Cendales, G. Dreibus, B. Spohel, V. Lorenz and H. Wanke, “The Abundances of Major, Minor and Traces Elements in the Earth’s Mantle as Derived from Primitive Ultramafic Nodules,” Lunar and Planetary Science Conference No. 10, Geochemical Acta, Suppl. 11, 1979, pp. 2031-2050.
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TITLE:
Petrochemical Characterization of Two Distinct Types of Dolerites from Bafoussam Area, West Cameroon
AUTHORS:
Gus Djibril Kouankap Nono, Pierre Wotchoko, Sylvestre Ganno, Divine Ngong Njinchuki, Jean Paul Nzenti
KEYWORDS:
Doleritic Dyke; Petrochemical; Alkaline; Tholeiitic; Intraplaque; Bafoussam
JOURNAL NAME:
International Journal of Geosciences,
Vol.4 No.8,
October
18,
2013
ABSTRACT:
Two petrochemical types of doleritic dykes have been distinguished in Bafoussam area: 1) the olivine-bearing dolerites which are the most representative are dark green, showing characteristics of alkaline basalts and, 2) the calcite-bearing dolerites are grayish green, showing characteristics of tholeiitic basalts. The studied dolerites are less differentiated (1 FeOt/MgO 2); they present the evolution of a subalkaline magma following a calc-alkaline series (alkaline dolerites) and the tholeiitic series (tholeitiic dolerite). The chondrite normalized multielement spider diagrams of all the dolerites show a pronounced depletion in Ba, Th, and enrichment in Rb. Their geotectonic context is inferred to be intraplate and the contrast between the two types is probably due to a diverse source: crustal source for calcite-bearing dolerites and mantle source for olivine-bearing dolerites.