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

作     者：Ulrich Verne Matiaba Bazika Vicky Tendresse Télange Bouénitéla Nelson Makamba Lekeba Florent Boudzoumou Ulrich Verne Matiaba Bazika;Vicky Tendresse Télange Bouénitéla;Nelson Makamba Lekeba;Florent Boudzoumou

作者机构：Laboratoire de géodynamique Faculté des Sciences et Techniques Université Marien Ngouabi Brazzaville Congo Département des Géosciences Institut National de Recherches en Sciences Exacts et Naturelles Brazzaville Congo 

出 版 物：《Open Journal of Geology》 (地质学期刊（英文）)

年 卷 期：2022年第12卷第11期

页      面：919-946页

学科分类：0709[理学-地质学] 070901[理学-矿物学、岩石学、矿床学] 07[理学] 

主　　题：Nemba Complex Mayombe Loukounga Greenstone Geodynamic Context Mantle Plumes 

摘      要：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.