Petrogenesis of the Sabongari alkaline complex, cameroon line (central Africa): Preliminary petrological and geochemical constraints

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• 作者：Emmanuel Njonfang^a ; ^{enjonfang@yahoo.fr} ; Gilbert Tchuenté ; Tchoneng^b ; Domenico Cozzupoli^c ; Federico Lucci^c
• 关键词：Sabongari complex ; Tikar plain ; Bimodal series ; Aluminous trend ; Peralkaline trend ; Fractional crystallization
• 刊名：Journal of African Earth Sciences
• 出版年：2013
• 出版时间：July, 2013
• 年：2013
• 卷：83
• 期：Complete
• 页码：25-54
• 全文大小：1814 K

文摘

The petrography, mineral chemistry and geochemical features of the Sabongari alkaline complex are presented and discussed in this paper with the aim of constraining its petrogenesis and comparing it with other alkaline complexes of the Cameroon Line. The complex is mainly made up of felsic rocks: (i) granites predominate and include pyroxene-amphibole (the most abundant), amphibole-biotite, biotite and pyroxene types; (ii) syenites are subordinate and comprise amphibole-pyroxene and amphibole-biotite quartz syenites; (iii) pyroxene-amphibole-biotite trachyte and (iv) relatively abundant rhyolite. The minor basic and intermediate terms associated with felsic rocks consist of basanites, microdiorite and monzodioites. Two groups of pyroxene bearing rocks are distinguished: a basanite-trachyte-granite (Group 1) bimodal series (SiO₂ gap: 44 and 63 wt. % ) and a basanite-microdiorite-monzodiorite-syenite-granite (Group 2) less pronounced bimodal series (reduced SiO₂ gap: 56-67 wt. % ). Both are metaluminous to peralkaline whereas felsic rocks bare of pyroxene (Group 3) are metaluminous to peraluminous. The Group 1 basanite is SiO₂-undersaturated (modal analcite in the groundmass and 11.04 wt. % normative nepheline); its Ni (240 ppm) and Cr (450 ppm) contents, near mantle values, indicate its most primitive character. The Group 2 basanite is rather slightly SiO₂-saturated (1.56 wt. % normative hypersthene), a marker of its high crustal contamination (low Nb/Y-high Rb/Y). The La/Yb and Gd/Yb values of both basanites (1: 19.47 and 2.92; 2: 9.09 and 2.23) suggest their common parental magma composition, and their crystallization through two episodes of partial melting (2 % and 3 % respectively) of a lherzolite mantle source with <4 % residual garnet. The effects of crustal contamination were selectively felt in the values of HFSE/LREE, LREE/LILE and LREE/HFSE ratios, known as indicators. Similar features have been recently obtained in the felsic lavas of the Cameroon Volcanic Line.