 | | Journal (article/letter/editorial) | | response to hydrothermal alteration at Mount Etinde, Cameroon Jacques Etame a,∗ , Che Emmanuel Suh b...Douala, Faculty of Sciences, BP 24157, Douala, Cameroon Economic Geology Unit, Department of Geology and...Environmental Science, University of Buea, P.O. Box 63, Buea, Cameroon c IRD, UMR 161 CEREGE, Institut de...rocks and hydrothermally altered rocks at Mount Etinde (Cameroon Volcanic Line, West Africa) have been studied...(1995) described the nephelinitic rocks at Mount Etinde Cameroon as Quaternary rocks which have been subjected |  | Yamgouot, Fadimatou Ngounouno, Déruelle, Bernard, Gbambié Mbowou, Isaac Bertrand, Ngounouno, Ismaïla, Demaiffe, Daniel (2016) Geochemistry of the volcanic rocks from Bioko Island (“Cameroon Hot Line”): Evidence for plume-lithosphere interaction. Geoscience Frontiers, 7 (5) 743-757 doi:10.1016/j.gsf.2015.06.003 | Journal (article/letter/editorial) | | Geochemistry of the volcanic rocks from Bioko Island (“Cameroon Hot Line”): Evidence for plume-lithosphere interaction...Université de Ngaoundéré, B.P. 454, Ngaoundéré, Cameroon Laboratoire de Magmatologie et Géochimie Inorganique...Université de Ngaoundéré, B.P. 115, Meiganga, Cameroon d Laboratoire de Géochimie Isotopique et Géodynamique...the presently more active volcanic zone of the Cameroon Line and composed essentially of alkaline basalts...geochemical signatures are similar to those of the Mount Cameroon rocks, and might be attributed to low degrees |  | Mbassa, Benoît Joseph, Njonfang, Emmanuel, Benoit, Mathieu, Kamgang, Pierre, Grégoire, Michel, Duchene, Stephanie, Brunet, Pierre, Ateba, Bekoa, Tchoua, Félix M. (2012) Mineralogy, geochemistry and petrogenesis of the recent magmatic formations from Mbengwi, a continental sector of the Cameroon Volcanic Line (CVL), Central Africa. Mineralogy and Petrology, 106 (3) 217-242 doi:10.1007/s00710-012-0227-5 | Journal (article/letter/editorial) | | formations from Mbengwi, a continental sector of the Cameroon Volcanic Line (CVL), Central Africa Benoît Joseph...et Minières, IRGM/ARGV Ekona, B.P. 370, Buéa, Cameroon E. Njonfang Laboratoire de Géologie, Ecole Normale...Supérieure, Université de Yaoundé I, B.P. 47 Yaoundé, Cameroon M. Benoit : M. Grégoire (*) : S. Duchene : P....Sciences, Université de Yaoundé I, B.P. 812, Yaoundé, Cameroon in a trachyte from neighboring Bamenda Mountains...parental magmas along the CVL. Introduction The Cameroon volcanic line (CVL) is a tectono-magmatic structure |  | | Book | | ring complexes and the chapter devoted to the Cameroon line. A detailed review of African ring complexes... XIV 2 Contents Phanerozoic Volcanism of Southwest Uganda: A Case for Regional K and lile Enrichment...Ultrapotassic Mafic-Ultramafic Magmatism in the Southwest Uganda Region of the African Rift: Implications from...Mafic-Ultramafic Ultra potassic Rocks of the Southwest Ugandan Area ........................... 3 Inferences.... . . ... 3 The Crust Under the Canary Islands Region ............. 4 Network of Fractures and Identity |  | Melluso, L., Tucker, R.D., Cucciniello, C., le Roex, A.P., Morra, V., Zanetti, A., Rakotoson, R.L. (2018) The magmatic evolution and genesis of the Quaternary basanite-trachyphonolite suite of Itasy (Madagascar) as inferred by geochemistry, Sr-Nd-Pb isotopes and trace element distribution in coexisting phases. Lithos, 310. 50-64 doi:10.1016/j.lithos.2018.04.003 | Journal (article/letter/editorial) | | d’Ambre/Bobaomby, Massif d’Ambre) to the southwest (Ankililoaka, Tulear region; NU Fig. 1a). This volcanism is...and after formation of the lacustrine basins, the region is believed to MA have experienced regional E-W...rocks (Supplementary Clinopyroxene ranges from diopside [Mg#=82, TiO2=1.3 wt.%; Mg# is 100Mg/(Mg+Fe)]...basanites (4.2-4.8) indicate a highly enriched source region (Melluso et al., 2016 and references therein)....and Schmincke, 1984; Tenerife: Bryan, 2006; Mt. Etinde: Nkombou et al., 1995; Mt. Vulture: Beccaluva et |
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