Improving geochronological framework of the Pan-African orogeny in Cameroon: New SIMS zircon and monazite U-Pb age constraints

• Published in: Precambrian research Vol. 294; pp. 307 - 321
• Main Authors: Li, Xian-Hua, Chen, Yi, Tchouankoue, Jean Pierre, Liu, Chuan-Zhou, Li, Jiao, Ling, Xiao-Xiao, Tang, Guo-Qiang, Liu, Yu
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.06.2017
• Subjects: Granite; Granulite facies metamorphism; Hf and O isotopes; Neoproterozoic Fold Belt of Cameroon; Pan-African orogeny; SIMS zircon and monazite U-Pb age; SIMS zircon and monazite U-Pb age; Hf and O isotopes; Pan-African orogeny; Granulite facies metamorphism; Granite; Neoproterozoic Fold Belt of Cameroon
• ISSN: 0301-9268; 1872-7433
• DOI: 10.1016/j.precamres.2017.04.006

•In situ U-Pb and Hf-O isotopes were analyzed for orthogneiss, leucosome and granite rocks from NFBC.•Syn-D2 magamtism and metamorphism took place at 620–610Ma.•Syn- and post-D4 granites are dated respectively at 561 and 557Ma.•≥620Ma, 620–600Ma, 590–580Ma and 560Ma correspond to respectively D1, D2, D3 and D4 phases. High-precision geochronological framework is crucial to understanding of the evolution of orogenesis. As part of the Pan-African North Equatorial Fold Belt, the Neoproterozoic Fold Belt of Cameroon (NFBC) involved polyphase deformation (D1 to D4 phases), metamorphism (up to granulite facies) and widespread crustal anatexis and magmatism. While a general geochronological framework has been established, controversy still exists on the temporal evolution of the metamorphic and magmatic events associated with polyphase deformation, in particular, the accurate age and geodynamic manifestations underlining the end of the orogeny are yet to be well constrained. We conduct in this work integrated analyses of SIMS U-Pb zircon and monazite dating and in-situ zircon Hf-O isotopes on the orthogneiss, leucosome and granite samples from Wum and Yaoundé of southwestern Cameroon in order to provide further constraints on temporal evolution of the NFBC. Our high-precision SIMS U-Pb age data demonstrate that the magmatic protoliths of orthogneisses from Wum and Yaoundé were emplaced synchronously at ca. 620Ma. They were generated by partial melting of the thickened Paleoproterozoic crustal basement rocks with zircon Hf TDMc model age of ca. 1.9–2.0Ga. Metamorphic zircons and two generations of monazites from an in-situ leucosome within the granulitic paragneiss of the Yaoundé Group yield indistinguishable ages of ca. 610Ma. These new results, in combination with previous isotopic data, suggest that the Yaoundé Group supracrustal rocks with zircon Hf TDMc model age of ca. 1.7Ga experienced a very rapid evolution from sedimentation at <626Ma, burial to deformation and granulite facies metamorphism at ca. 610Ma. The deformed two-mica granite and undeformed biotite granite in Wum were precisely dated at 561±3Ma and 557±4Ma, respectively. They both were derived from similar supracrustal sources with zircon Hf TDMc model age of ca. 2.56–2.40Ga. On the basis of our new SIMS U-Pb ages, along with existing dates from the literature, an improved geochronological framework is proposed for the NFBC, with ages of ≥620Ma, ca. 620–600Ma, ca. 590–580Ma, and ca. 580–560Ma for the D1, D2, D3, and D4 phase events, respectively.