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Mantle sources beneath the Cameroon Volcanic Line: geochemistry and geochronology of the Bamoun plateau mafic rocks

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Abstract

The age and origin of the volcanism along the Cameroon Volcanic Line (CVL) are still a matter of debate. We present major and trace element compositions as well as Sr–Nd–Pb–Hf isotopic results for mafic rocks from the Bamoun area, in the central part of the Cameroon Volcanic Line, as well as for two samples from recent eruptions of Mt. Cameroon. Lava flows are mostly basalts and hawaiites with transitional affinity. Some samples are among the oldest rocks of the CVL, with ages older than 51 My while some rocks are very young, around 0.05 My. All the samples are enriched in incompatible elements, indicating that melts were formed in a garnet-bearing mantle source. Different mantle sources participated to the formation of the Bamoun lavas. One source is isotopically similar to the main volcanic rocks of the CVL and probably represents an important part of the subcontinental lithospheric mantle. The second source is enriched in incompatible elements and shows a marked positive Eu anomaly, probably related to the participation of pyroxenites in the partial melting processes. The third mantle source is similar to the source of the Mt. Cameroon. This mantle source was known previously only in the Mt. Cameroon lavas, and we report its occurrence for the first time in old lavas and in other location along the CVL.

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References

  • Adams AN, Wiens DA, Nyblade AA, Euler GG, Shore PJ, Tibi R (2015) Lithospheric instability and the source of the Cameroon Volcanic Line: evidence from Rayleigh wave phase velocity tomography. J Geophys Res 120:1708–1727

    Article  Google Scholar 

  • Anders E, Grevesse N (1989) Abundances of the elements: Meteoritic and solar. Geochim Cosmochim Acta 53:197–214

    Article  Google Scholar 

  • Ballentine CJ, Lee DC, Halliday AN (1997) Hafnium isotopic studies of the Cameroon Line and new HIMU paradoxes. Chem Geol 139:111–124

    Article  Google Scholar 

  • Barfod DN, Ballentine CJ, Halliday AN, Fitton JG (1999) Noble gases in the Cameroon line and the He, Ne, and Ar isotopic compositions of high μ (HIMU) mantle. J Geophys Res 104:29509–29527

    Article  Google Scholar 

  • Bellon H, Quoc Buü N, Chaumont J, Philippet JC (1981) Implantation ionique d'argon dans une cible support: application au traçage isotopique de l'argon contenu dans les minéraux et les roches. C R Acad Sci Paris 292:977–980

    Google Scholar 

  • Blichert-Toft J, Agranier A, Andres M, Kingsley R, Schilling JG, Albarède F (2005) Geochemical segmentation of the Mid-Atlantic Ridge north of Iceland and ridge-hot spot interaction in the North Atlantic. Geochem Geophys Geosys 6(1)

  • Chaffey DJ, Cliff RA, Wilson BM (1989) Characterization of the St. Helena Magma Source Magmatism in the Ocean Basins. In: Saunders, A.D. and Norry, M.J. (Eds.) Geological Society of London, London: 257–276.

  • Cotten J, Le Dez A, Bau M, Caroff M, Maury RC, Dulski P, Brousse R (1995) Origin of anomalous rare-earth element and yttrium enrichments in sub aerially exposed basalts: evidence from French Polynesia. Chem Geol 119:115–138

    Article  Google Scholar 

  • Cox A, Dalrymple GB (1967) Statistical analysis of geomagnetic reversal data and the precision of 865 potassium-argon dating. J Geophys Res 72:2603–2614

    Article  Google Scholar 

  • De Plaen RSM, Bastow ID, Chambers EL, Keir D, Gallacher RJ, Keane J (2014) The development of magmatism along the Cameroon Volcanic Line: evidence from seismicity and seismic anisotropy. J Geophys Res 119:4233–4252. doi:10.1002/2013JB010583

    Article  Google Scholar 

  • Fitton JG, Dunlop HM (1985) The Cameroon line, West Africa, and its bearing on the origin of oceanic and continental alkali basalt. Earth Planet Sci Lett 72:23–38

    Article  Google Scholar 

  • Fourel L, Milelli L, Jaupart C, Limare A (2013) Generation of continental rifts, basins, and swells by lithosphere instabilities. J Geophys Res Solid Earth 118:3080–3100. doi:10.1002/jgrb.50218

    Article  Google Scholar 

  • Halliday AN, Dickin AP, Fallick AE, Fitton JG (1988) Mantle dynamics: a Nd, Sr, Pb and O isotopic study of the Cameroon line volcanic chain. J Petrol 29:181–211

    Article  Google Scholar 

  • Irvine TN, Baragar WRA (1971) A guide to the chemical classification of the common volcanic rocks: Can J Earth Sci 523-548.

  • Kamgang P, Njonfang E, Chazot G, Tchoua FM (2007) Géochimie et géochronologie des laves felsiques des monts Bamenda (ligne volcanique du Cameroun). C R Géoscience 339:659–666

    Article  Google Scholar 

  • Kamgang P, Chazot G, Njonfang E, Tchoua FM (2008) Geochemistry andgeochronology of mafic rocks from Bamenda Mountains (Cameroon): Source composition and crustal contamination along the Cameroon Volcanic Line. C R Géoscience 340:850–857

    Article  Google Scholar 

  • Kamgang P, Chazot G, Njonfang E, Ngongang NBT, Tchoua FM (2013) Mantle sources and magma evolution beneath the Cameroon Volcanic Line: geochemistry of mafic rocks from the Bamenda Mountains (NW Cameroon). Gond Res 24:727–741

    Article  Google Scholar 

  • Le Bas MJ, Le Maitre RW, Streckeisen A, Zanettin B (1986) A chemical classification of volcanic rocks based on the total alkali–silica diagram. J Petrol 27:745–750

    Article  Google Scholar 

  • Lee DC, Halliday AN, Fitton JG, Poli G (1994) Isotopic variation with distance and time in the volcanic islands of the Cameroon Line, evidence from mantle plume origin. Earth Planet Sci Lett 124:119–138

    Article  Google Scholar 

  • Li ZXA, Lee CTA (2006) Geochemical investigation of serpentinized oceanic lithospheric mantle in the Feather River Ophiolite, California: implications for the recycling rate of water by subduction. Chem Geol 235:161–185

    Article  Google Scholar 

  • Marzoli A, Renne PR, Piccirillo EM, Francesca C, Bellieni G, Melfi AJ, N'ni J (1999) Silicic magmas from the continental Cameroon Volcanic Line (Oku, Bambouto and Ngaoundere): 40Ar-39Ar dates, petrology, Sr-Nd-O isotopes and their petrogenetic significance. Contrib Mineral Petrol 135:133–150

    Article  Google Scholar 

  • Marzoli A, Peccirillo EM, Renne PR, Bellieni G, Iacumin M, Nyobe JB, Tongwa AT (2000) The Cameroon Volcanic Line revisited: petrogenesis of continental basaltic magmas from lithospheric and asthenospheric mantle sources. J Petrol 41:87–109

    Article  Google Scholar 

  • Milelli L, Fourel L, Jaupart C (2012) A lithospheric instability origin for the CameroonVolcanic Line. Earth Planet Sci Let 335–336:80–87

    Article  Google Scholar 

  • Moundi A, Menard JJ, Reusser E, Tchoua F, Dietrich VJ (1996) Découverte de basaltes transitionnels dans le secteur continental de la Ligne du Cameroun (Massif du Mbam, Ouest-Cameroun). C R Acad Sci 322:831–837

    Google Scholar 

  • Moundi A, Wandji P, Bardintzeff JM, Ménard JJ, Okomo Atouba LC, Mouncherou OF, Reusser E, Bellon H, Tchoua FM (2007) Les basaltes éocènes à affinité transitionnelle du plateau Bamoun, témoins d’un réservoir mantellique enrichi sous la Ligne Volcanique du Cameroun. C R Geosci 339:396–406

    Article  Google Scholar 

  • Moundi A, Njilah IK, Ghogomu RT, Wokwenmendam NP (2008) New geochronological Data on the Continental Alkaline Flood Basalts of the Bamoun Plateau: evidence of an early Alkaline Volcanism of the Cameroon Line. Disaster Advances 1:27–33

    Google Scholar 

  • Moundi A, Wandji P, Ghogomu RT, Bardintzeff JM, Njilah IK, Foumboure I, Ntieche B (2009) Existence of Quaternary ankaramites among tertiary floods basalts at Koutaba (Bamoun Plateau, Western Cameroon): petrology and isotope data. Rev Bulgarian Geol Soc 70:115–124

    Google Scholar 

  • Rankenburg K, Lassiter JC, Brey G (2005) The role of continental crust and lithospheric mantle in the genesis of Cameroon volcanic line lavas: constraints from isotopic variations in lavas and megacrysts from the Biu and Jos Plateaux. J Petrol 46:169–190

    Article  Google Scholar 

  • Reusch AM, Nyblade AA, Wiens DA, Shore PJ, Ateba B, Tabod CT, Nnange JM (2010) Upper mantle structure beneath Cameroon from body wave tomography and the origin of the Cameroon Volcanic Line. Geochem Geophys Geosyst 11 doi: 10.1029/2010GC003200

  • Reusch A, Nyblade A, Tibi R, Wiens D, Shore P, Bekoa A, Tabod C, Nnange J (2011) Mantle transition zone thickness beneath Cameroon: evidence for an upper mantle origin for the Cameroon Volcanic Line. Geophys J Inter 187:1146–1150

    Article  Google Scholar 

  • Steiger RH, Jäger E (1977) Subcommission on geochronology: convention on the use of decay 1112 constants in geo- and cosmochronology. Earth Planet Sci Let 36:359–362

    Article  Google Scholar 

  • Suh CE, Luhr JF, Njome MS (2008) Olivine-hosted glass inclusions from scoriae erupted in 1954–2000 at Mount Cameroon volcano, West Africa. J Volcanol Geotherm Res 169:1–33

    Article  Google Scholar 

  • Sun, S.S. and McDonough, W.F. (1989) Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. Geological Society, London, Special Publications 42: 313-345

  • Tchuimegnie Ngongang NB, Kamgang P, Chazot G, Agranier A, Bellon H, Nonnotte P (2015) Age, geochemical characteristics and petrogenesis of Cenozoic intraplate alkaline volcanic rocks in the Bafang region, West Cameroon. J Afr Earth Sci 102:218–232

    Article  Google Scholar 

  • Tsafack JPF, Wandji P, Bardintzeff JM, Bellon H, Guillou H (2009) The Mount Cameroon stratovolcano (Cameroon Volcanic Line, Central Africa): Petrology, geochemistry, isotope and age data. Mineral Petrol 47:65–78

    Google Scholar 

  • Wang K, Plank T, Walker JD, Smith EI (2002) A mantle melting profile across the basin and range, SW USA. J Geophys Res 107:1–21

    Google Scholar 

  • Yokoyama T, Festus Aka T, Kusakabe M, Nakamura E (2007) Plume-lithosphere interaction beneath Mt. Cameroon volcano, West Africa: constraints from 238U-230Th 226Ra and Sr-Nd-Pb isotope systematics. Geochim Cosmochim Acta 71:1835–1854

    Article  Google Scholar 

Download references

Acknowledgments

The authors would like to thank Andrea Marzoli and two anonymous reviewers for their constructive reviews which improved the quality of our manuscript.

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Correspondence to Gilles Chazot.

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Atouba, L.C.O., Chazot, G., Moundi, A. et al. Mantle sources beneath the Cameroon Volcanic Line: geochemistry and geochronology of the Bamoun plateau mafic rocks. Arab J Geosci 9, 270 (2016). https://doi.org/10.1007/s12517-015-2285-6

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