中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Early Cretaceous magmatism in Yunnan traces the tectonic transition from the Tengchong-Baoshan continental collision to Neo-Tethyan slab rollback

文献类型:期刊论文

作者Zhang, Jiuyuan5,6; Fan, Weiming2,6; Xu, Xi5; Peng, Touping1,3; Ratschbacher, Lothar4; Wang, Baodi5
刊名LITHOS
出版日期2023-11-01
卷号456页码:16
关键词Early Cretaceous Tengchong Block Adakitic rocks Geochemical transitions Tethys evolution
ISSN号0024-4937
DOI10.1016/j.lithos.2023.107316
英文摘要Early Cretaceous magmatic rocks of the Tengchong and Baoshan blocks provide insight into the late Mesozoic evolution of southeastern Tibet-Yunnan. We present LA-ICP-MS U-Pb zircon age, zircon eHf(t) isotope, and whole-rock geochemical and Sr-Nd isotopic data for dioritic porphyrite and rhyolite, outcropping in the Eastern Tengchong Belt and the Gaoligong Belt, respectively. The dioritic porphyrite has a 123.0 +/- 1.3 Ma (2 sigma) age, negative whole-rock (epsilon Nd)(t) of 1.99 to 2.16, initial Sr-87/Sr-86 of 0.70690-0.70734, zircon (epsilon Hf)(t) of 1.42 to 4.11, and adakitic geochemical features, suggesting an origin from mixing of mantle- and crust-derived magmas; the rhyolite has a 122.2 +/- 1.0 Ma age, low whole-rock (epsilon Nd)(t) of 9.69 to 8.83, initial Sr-87/Sr-86 of 0.71104-0.71246, and zircon (epsilon Hf)(t) of 8.55 to 2.59, suggesting crustal derivation. Our data-along with the published data-suggest that the Early Cretaceous rocks (140-109 Ma) comprise two magmatic phases with a geochemical and isotopic transition at similar to 123 Ma. The 140-123 Ma phase-mainly outcropping in the Gaoligong Belt-is mainly peraluminous, highly silicic, and has negative zircon (epsilon Hf)(t) values, suggesting derivation from remelting of ancient crust in a postcollisional setting; the 123-109 Ma phase is mainly metaluminous, restricted to the Eastern Tengchong Belt, and formed in a continental-arc setting with mantle melt involved. We propose that the similar to 123 Ma geochemical and isotopic change marks the transition from contraction due to the Tengchong-Baoshan collision to extension resulting from slab rollback of the Neo-Tethyan lithospheric slab.
WOS研究方向Geochemistry & Geophysics ; Mineralogy
语种英语
WOS记录号WOS:001081414900001
源URL[http://ir.gig.ac.cn/handle/344008/78886]  
专题同位素地球化学国家重点实验室
通讯作者Zhang, Jiuyuan; Fan, Weiming
作者单位1.Chinese Acad Sci, Ctr Excellence Deep Earth Sci, Guangzhou 510640, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China
4.TU Bergakad Freiberg, Geol, D-09599 Freiberg, Germany
5.China Geol Survey, China Aero Geophys Survey & Remote Sensing Ctr Na, Beijing 100083, Peoples R China
6.Chinese Acad Sci, Inst Tibetan Plateau Res, State Key Lab Tibetan Plateau Earth Syst Environm, Beijing 100101, Peoples R China
推荐引用方式
GB/T 7714
Zhang, Jiuyuan,Fan, Weiming,Xu, Xi,et al. Early Cretaceous magmatism in Yunnan traces the tectonic transition from the Tengchong-Baoshan continental collision to Neo-Tethyan slab rollback[J]. LITHOS,2023,456:16.
APA Zhang, Jiuyuan,Fan, Weiming,Xu, Xi,Peng, Touping,Ratschbacher, Lothar,&Wang, Baodi.(2023).Early Cretaceous magmatism in Yunnan traces the tectonic transition from the Tengchong-Baoshan continental collision to Neo-Tethyan slab rollback.LITHOS,456,16.
MLA Zhang, Jiuyuan,et al."Early Cretaceous magmatism in Yunnan traces the tectonic transition from the Tengchong-Baoshan continental collision to Neo-Tethyan slab rollback".LITHOS 456(2023):16.

入库方式: OAI收割

来源:广州地球化学研究所

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