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• W3197466734 abstract "The Pan-African/Brasiliano orogenic belts are a partof numerous Neoproterozoic orogenic belts that belong to the long-lived orgeniccycle that distancing phase started at the Tonian around 1.0 Ga. The Tonian magmatismfairly documented in the Neoproterozoic belts of Borborema Province(NE-Brazil), seemed so far inexistent in the Central African Orogenic Belt(CAOB) although these two belts were geologically correlated. Through the Lu-Hfgeochronological analysis on zircon of tonalite, the present work, coupled withthe previous data, suggests the existence of a Tonian age magmatism in theCentral Cameroon Domain of the CAOB although the latter is much reworked. TheNguesseck tonalite outcrops in the northern part of the Mbe-Sassa-Mbersi region, in the northern edge of CentralCameroon Domain of the CAOB and in the Tchollire-Banyo shear zone (TBSZ). The Lu-Hf data obtain onthe zircon grains of this tonalite reveal juvenile HfTDM age of ca.1.0 Ga. This age, combined to the previous geochemical data suggests that the protholites of this tonalite would haveextracted from the source during the distancing phase (rifting andoceanization) of the Pan-african/Brasiliano orogeny at the early Neoproterozoic." @default.
• W3197466734 created "2021-09-13" @default.
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• W3197466734 date "2021-01-01" @default.
• W3197466734 modified "2023-10-16" @default.
• W3197466734 title "Lu-Hf Isotopic Data of the Mb&#233;-Sassa-Mbersi Tonalite (Central Cameroon Domain): Indicator of ca. 1.0 Ga Juvenile Tonian Magmatism in the Region" @default.
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• W3197466734 doi "https://doi.org/10.4236/gep.2021.99001" @default.
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