Piccirillo, E.M., Comin-Chiaramonti, P., Melfi, A.J., Stolfa, D., Bellieni, G., Marques, L.S., Giaretta, A., Nardy, A.J.R., Pinese, J.P.P., Raposo, M.I.B. and Roisenberg, A. (1988) Petrochemistry of Continental Flood Basalt-Rhyolite Suites and Related Intrusives from the Parana Basin (Brazil). In: Piccirillo, E.M. and Melfi, A.J., Eds., The Mesozoic Flood Volcanism of the Paraná Basin: Petrogenetic and Geophysical Aspects, Instituto Astronomica e Geofisico Publishers, IAG-USP Press, Sao Paulo, 107-156.
https://doi.org/10.1007/978-94-015-7805-9_6

has been cited by the following article:

• TITLE: Petrology and Geochemistry of Loukounga Metabasites Rocks: Constraining the Geodynamic Context of Neoproterozoic Nemba Complex in the Mayombe Belt

  AUTHORS: Ulrich Verne Matiaba Bazika, Vicky Tendresse Télange Bouénitéla, Nelson Makamba Lekeba, Florent Boudzoumou

  KEYWORDS: Nemba Complex, Mayombe, Loukounga, Greenstone, Geodynamic Context, Mantle Plumes

  JOURNAL NAME: Open Journal of Geology, Vol.12 No.11, November 16, 2022

  ABSTRACT: This study focuses on the metabasite rocks of the Nemba Complex of the Mayombe belt, an African segment of Araçuaï-West Congo Orogen (A-WCO) extending from the southwest of Gabon to the northwest of Angola. These metabasite rocks outcrops are in southwestern Congo along the Loukounga river. The Nemba complex is of Neoproterozoic age and represents the lower part of the west congolian Supergroup. The objective of this study is to constrain the geodynamic context of the Nemba complex from the petrology and geochemistry of the metabasites sampled in the Loukounga River. The observed rocks are composed of amphibolites, metagabbros, epidotites and greenschists and are affected by folding accompanied by flux schistosity and crenulation schistosity. Geochemical analyzes show that the rocks have a basic to ultrabasic chemical composition with SiO2 contents between 41.85% and 58.23%. The geochemical composition of the major and traces elements shows that the rocks are basalts, basaltic andesites and andesites. The magma shows enrichment in LREE, LILE and depletion in HREE and HFSE. The multielement spectra show negative anomalies in Nb-Ta, Ti and a relatively low Nb/La ratio which characterize a lithospheric source contaminated by continental crust. Traces elements discrimination plots show that Loukounga metabasites are emplaced in intraplate geodynamic context like that associated with the basalts of the trap-types continental shelves and are possibly derived from mantle plumes contemporaneous with or slightly prior to magmatism.