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Geochemical characteristics and origin of the Neoproterozoic high-K calc-alkaline granitoids in the northern part of Mandara hills,northeastern Nigeria

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Acta Geochimica 2020年第3期39卷 337-354页

作者： Musa B.Girei tavershima najime Paul O.Ogunleye State Key Laboratory of Geological Processes and Mineral Resources Faculty of Earth ResourcesChina University of GeosciencesWuhan 430074China Department of Geology Faculty of Earth and Environmental Sciences.Bayero UniversityKanoNigeria Department of Geology Ahmadu Bello UniversityZariaNigeria Centre for Energy Research and Training Ahmadu Bello UniversityP.M.B.1014ZariaNigeria

The high-K calc-alkaline granitoids in the northern part of the Mandara Hills are part of the wellexposed post-collisional plutons in northeastern *** calc-alkaline rock association consists of quartz monzodiorite,hornblende biotite granite,biotite granites and aplite which intruded the older basement consisting mainly of low-lying migmatitic gneisses and amphibolites during the Neoproterozoic Pan-African *** and geochemical studies have revealed the presence of hornblende,iron oxide,and metaluminous to slightly peraluminous characteristics in the granitoids which is typical of I-type *** granitoids are also depleted in some high field strength elements(*** and Ta) as well as *** of Mg#versus SiO2 indicate that the granite was derived from partial melting of crustal *** delamination at the waning stage of the PanAfrican Orogeny possibly triggered upwelling of hot mafic magma from the mantle which underplated the lower ***,in turn,caused partial melting and magma generation at the lower to middle-crustal ***,the peculiar geochemical characteristics of the quartz monzodiorite especially the enrichment in compatible elements such as MgO,Cr,and Ni,as well as LILE element(e.g.K,Ce,Cs,Ba,and Sr),signify that the rock formed from an enriched upper mantle *** emplacement of high-K granites in the Madara Hill,therefore,marked an important episode of crustal reworking during the ***,further isotopic work is needed to confirm this model.

关键词： Calc-alkaline I-type granitoids Pan-African Mandara hills Nigeria

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