Marzoli, A., Renne, P. & Piccirillo, E.M. 1997. Ar/Ar data on volcanics of the continental Cameroon Line (Africa): time related migration of trachytic volcanism. Plinius, 18, 141-142.

Fitton, J. G., & Dunlop, H. M. (1985). The Cameroon line, West Africa, and its bearing on the origin of oceanic and continental alkali basalt. Earth and Planetary Science Letters, 72(1), 23-38. doi.org/10.1016/0012-821X(85)90114-1

Fitton, J. G. (1987). The Cameroon line, West Africa: a comparison between oceanic and continental alkaline volcanism. Geological Society, London, Special Publications, 30(1), 273-291.

Halliday, A. N., Dickin, A. P., Fallick, A. E., & Fitton, J. G. (1988). Mantle dynamics: a Nd, Sr, Pb and O isotopic study of the Cameroon line volcanic chain. Journal of Petrology, 29(1), 181-211. doi.org/10.1093/petrology/29.1.181

Le Guern, F. & Sigvaldason, G. (1989). The lake Nyos event and natural CO2 degassing. J. Volcanol. Geoth. Res (Special Issue), 2-3, 97-275.

Déruelle, B., Moreau, C., Nkoumbou, C., Kambou, R., Lissom, J., Njonfang, E., ... & Nono, A. (1991). The Cameroon line: a review. In Magmatism in extensional structural settings (pp. 274-327). Springer, Berlin, Heidelberg.

Lee, D. C., Halliday, A. N., Davies, G. R., Essene, E. J., Fitton, J. G., & Temdjim, R. (1996). Melt enrichment of shallow depleted mantle: a detailed petrological, trace element and isotopic study of mantle-derived xenoliths and megacrysts from the Cameroon Line. Journal of Petrology, 37(2), 415-441. doi.org/10.1093/petrology/37.2.415

Ballentine, C. J., Lee, D. C., & Halliday, A. N. (1997). Hafnium isotopic studies of the Cameroon line and new HIMU paradoxes. Chemical Geology, 139(1-4), 111-124. doi.org/10.1016/S0009-2541(97)00028-4

Marzoli, A., Piccirillo, E. M., Renne, P. R., Bellieni, G., Iacumin, M., Nyobe, J. B., & Tongwa, A. T. (2000). The Cameroon Volcanic Line revisited: petrogenesis of continental basaltic magmas from lithospheric and asthenospheric mantle sources. Journal of petrology, 41(1), 87-109. doi.org/10.1093/petrology/41.1.87

Reference Search (possible matching items)

	Kamgang, Pierre, Chazot, Gilles, Njonfang, Emmanuel, Ngongang, Nicaise Blaise Tchuimegnie, Tchoua, Félix M. (2013) Mantle sources and magma evolution beneath the Cameroon Volcanic Line: Geochemistry of mafic rocks from the Bamenda Mountains (NW Cameroon) Gondwana Research, 24 (2) 727-741 doi:10.1016/j.gr.2012.11.009	Journal (article/letter/editorial)
	beneath the Cameroon Volcanic Line: Geochemistry of maﬁc rocks from the Bamenda Mountains (NW Cameroon) Pierre...December 2012 Handling Editor: I. Safonova Keywords: Cameroon Volcanic Line Bamenda Mountains Maﬁc lavas Crustal...rocks from the Bamenda Mountains, part of the Cameroon Volcanic Line (CVL), in order to discuss the origin...continental intraplate tectonic settings. The Cameroon Volcanic Line (CVL) is a chain of 12 Cenozoic...continent/ocean boundary (c.o.b.: Bioko, Etinde and Mt. Cameroon) and the continental sector. The continental sector
	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
	Nkouandou, O. F., Temdjim, R. (2011) Petrology of spinel lherzolite xenoliths and host basaltic lava from Ngao Voglar volcano, Adamawa Massif (Cameroon Volcanic Line, West Africa): equilibrium conditions and mantle characteristics. Journal of GEOsciences, 56 (4) 375-387	Journal (article/letter/editorial)
	basaltic lava from Ngao Voglar volcano, Adamawa Massif (Cameroon Volcanic Line, West Africa): equilibrium conditions...University of Ngaoundere, P.O. Box 454 Ngaoundere, Cameroon Department of Earth Sciences, Faculty of Sciences...University of Yaounde I, P.O. Box 812 Yaoundé, Cameroon; rtemdjim@yahoo.fr Corresponding author Spinel-bearing...Voglar volcano, 35 km northwest of Ngaoundere in the Adamawa volcanic Massif (Cameroon). They have been examined...conditions of the upper mantle beneath the Ngaoundere region. The xenoliths exhibit protogranular textures and
	*(1991) Magmatism in Extensional Structural Settings. Springer Berlin Heidelberg. doi:10.1007/978-3-642-73966-8*	Book
	ring complexes and the chapter devoted to the Cameroon line. A detailed review of African ring complexes...Mafic-Ultramafic Magmatism in the Southwest Uganda Region of the African Rift: Implications from Experimental...146 146 5 The Mesozoic Tholeiitic Province of Northwest Africa: A Volcanotectonic Record of the Early.... . . ... 3 The Crust Under the Canary Islands Region ............. 4 Network of Fractures and Identity...Identity of Vertical Movements in the Canary Islands Region ........................... 4.1 Transoceanic and

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Fayalite from Oku Massif, Northwest Region, Cameroon

Fayalite from
Oku Massif, Northwest Region, Cameroon