中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Improving geochronological framework of the Pan-African orogeny in Cameroon: New SIMS zircon and monazite U-Pb age constraints

文献类型:期刊论文

作者Li, Xian-Hua1,2; Chen, Yi1; Tchouankoue, Jean Pierre3; Liu, Chuan-Zhou1,4; Li, Jiao1; Ling, Xiao-Xiao1; Tang, Guo-Qiang1,2; Liu, Yu1,2
刊名PRECAMBRIAN RESEARCH
出版日期2017-06-01
卷号294页码:307-321
关键词Sims Zircon And Monazite U-pb Age Hf And o Isotopes Granulite Facies Metamorphism Granite Neoproterozoic Fold Belt Of Cameroon Pan-african Orogeny
ISSN号0301-9268
DOI10.1016/j.precamres.2017.04.006
文献子类Article
英文摘要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 Yaounde 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 Yaounde were emplaced synchronously at ca. 620 Ma. They were generated by partial melting of the thickened Paleoproterozoic crustal basement rocks with zircon Hf T-DM(c) model age of ca. 1.9-2.0 Ga. Metamorphic zircons and two generations of monazites from an in-situ leucosome within the granulitic paragneiss of the Yaounde Group yield indistinguishable ages of ca. 610 Ma. These new results, in combination with previous isotopic data, suggest that the Yaounde Group supracrustal rocks with zircon Hf T-DM(c) model age of ca. 1.7 Ga experienced a very rapid evolution from sedimentation at < 626 Ma, burial to deformation and granulite facies metamorphism at ca. 610 Ma. The deformed two-mica granite and undeformed biotite granite in Wum were precisely dated at 561 +/- 3 Ma and 557 +/- 4 Ma, respectively. They both were derived from similar supracrustal sources with zircon Hf T-DM(c) model age of ca. 2.56-2.40 Ga. 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 >= 620 Ma, ca. 620-600 Ma, ca. 590-580 Ma, and ca. 580-560 Ma for the D1, D2, D3, and D4 phase events, respectively. (C) 2017 Elsevier B.V. All rights reserved.
WOS关键词HF-O ISOTOPES ; NORTH-CENTRAL CAMEROON ; MC-ICP-MS ; FOLD BELT ; SOUTHERN CAMEROON ; WEST-CAMEROON ; SE CHINA ; LU-HF ; METAMORPHIC EVENTS ; WORKING REFERENCE
WOS研究方向Geology
语种英语
WOS记录号WOS:000402217500017
出版者ELSEVIER SCIENCE BV
资助机构Chinese Academy of Sciences(XDB18030300 ; Chinese Academy of Sciences(XDB18030300 ; QYZDY-SSW-DQC017) ; QYZDY-SSW-DQC017) ; Chinese Academy of Sciences(XDB18030300 ; Chinese Academy of Sciences(XDB18030300 ; QYZDY-SSW-DQC017) ; QYZDY-SSW-DQC017) ; Chinese Academy of Sciences(XDB18030300 ; Chinese Academy of Sciences(XDB18030300 ; QYZDY-SSW-DQC017) ; QYZDY-SSW-DQC017) ; Chinese Academy of Sciences(XDB18030300 ; Chinese Academy of Sciences(XDB18030300 ; QYZDY-SSW-DQC017) ; QYZDY-SSW-DQC017)
源URL[http://ir.iggcas.ac.cn/handle/132A11/52867]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Li, Xian-Hua
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China
3.Univ Yaounde I, Dept Earth Sci, POB 812, Yaounde, Cameroon
4.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
推荐引用方式
GB/T 7714
Li, Xian-Hua,Chen, Yi,Tchouankoue, Jean Pierre,et al. Improving geochronological framework of the Pan-African orogeny in Cameroon: New SIMS zircon and monazite U-Pb age constraints[J]. PRECAMBRIAN RESEARCH,2017,294:307-321.
APA Li, Xian-Hua.,Chen, Yi.,Tchouankoue, Jean Pierre.,Liu, Chuan-Zhou.,Li, Jiao.,...&Liu, Yu.(2017).Improving geochronological framework of the Pan-African orogeny in Cameroon: New SIMS zircon and monazite U-Pb age constraints.PRECAMBRIAN RESEARCH,294,307-321.
MLA Li, Xian-Hua,et al."Improving geochronological framework of the Pan-African orogeny in Cameroon: New SIMS zircon and monazite U-Pb age constraints".PRECAMBRIAN RESEARCH 294(2017):307-321.

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来源:地质与地球物理研究所

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