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Correlation among the Ailaoshan-Song Ma-Song Chay orogenic belts and implications for the evolution of the eastern Paleo-Tethys Ocean br
Wang, Yin1,2,3; Lin, Wei1,3; Faure, Michel4; Van Nguyen, Vuong5; Meng, Lingtong1,3; Chu, Yang1,3; Wei, Wei1,3; Thu, Hoai Luong Thi5; Lepvrier, Claude6; Van Vu, Tich5; Li, Qiuli1,3; Wang, Hao1,3; Chen, Zechao1,3; Wu, Lin1,3; Wang, Fei1,3
2022-11-20
Source PublicationTECTONOPHYSICS
ISSN0040-1951
Volume843Pages:22
AbstractThe timing and mechanism of the combination between the South China Block (SCB) and the Indochina Block (IB) are controversial. Three ophiolitic me ' lange zones (Ailaoshan, Song Ma, and Song Chay) have been proposed as suture zones within this collisional orogen. However, the relationships among the three corresponding tectonic belts are unclear. In this study, we present detailed structural data for the three tectonic belts. The bulk architectures of the Ailaoshan, Song Ma, and Song Chay belts correlate well with one another. This similarity is also revealed by our new zircon U-Pb geochronological results from the Song Ma and Song Chay ophiolites. The regional deformation age is constrained to between 250 and 240 Ma by our new muscovite 40Ar/39Ar ages, and the medium-low temperature conditions are revealed by the quartz c-axis fabric. Considering the transformation effect of the Cenozoic large-scale sinistral strike-slip of the RRF and DBF, the Early Mesozoic Ailaoshan, Song Ma, and Song Chay suture zones should represent different segments of the same belt. Based on this hypothesis, we compiled the ages of the magmatism in this region, which allows us to propose an evolutional model as follows: i) -380-310 Ma continental rifting and subsequent Ailaoshan-Song Ma-Song Chay ocean spreading as a branch of the Paleo-Tethys, ii) -310-250 Ma oceanic subduction coeval with continental-arc magmatism, iii) -250-240 Ma continental collision, iv) -240-220 Ma post-collisional extension.
KeywordStructural analysis Ailaoshan-Song Ma-Song Chay Paleo-Tethys Indosinian orogeny
DOI10.1016/j.tecto.2022.229618
Funding OrganizationNational Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China
WOS KeywordRIVER SHEAR ZONE ; ZIRCON U-PB ; ARC/BACK-ARC ASSEMBLAGES ; SEVIER-LARAMIDE OROGENY ; PLATE TECTONIC CYCLE ; INDO-CHINA BLOCKS ; SOUTH CHINA ; TRUONG-SON ; SUTURE ZONE ; NORTHERN VIETNAM
Language英语
Funding ProjectNational Natural Science Foundation of China ; National Key Research and Development Program of China ; [91855212] ; [2021YFB23013013] ; [2016YFC0600401]
Funding OrganizationNational Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China
WOS Research AreaGeochemistry & Geophysics
WOS SubjectGeochemistry & Geophysics
WOS IDWOS:000878612100001
PublisherELSEVIER
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Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/107730
Collection岩石圈演化国家重点实验室
Corresponding AuthorLin, Wei
Affiliation1.Chinese Acad Sci, Inst Geol & Geophys, Innovat Acad Earth Sci, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Sinopec Matrix Corp, Geosteering & Logging Res Inst, Qingdao 266071, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
4.Univ Orleans, Inst Sci Terre Orleans, UMR 7327, CNRS, F-45067 Orleans 2, France
5.Hanoi Univ Sci, Fac Geol, Hanoi, Vietnam
6.Univ Paris 06, Inst Sci Terre Paris, UMR 7193, CNRS, Case 129, F-75252 Paris 05, France
First Author AffilicationInstitute of Geology and Geophysics, Chinese Academy of Sciences
Corresponding Author AffilicationInstitute of Geology and Geophysics, Chinese Academy of Sciences
Recommended Citation
GB/T 7714
Wang, Yin,Lin, Wei,Faure, Michel,et al. Correlation among the Ailaoshan-Song Ma-Song Chay orogenic belts and implications for the evolution of the eastern Paleo-Tethys Ocean br[J]. TECTONOPHYSICS,2022,843:22.
APA Wang, Yin.,Lin, Wei.,Faure, Michel.,Van Nguyen, Vuong.,Meng, Lingtong.,...&Wang, Fei.(2022).Correlation among the Ailaoshan-Song Ma-Song Chay orogenic belts and implications for the evolution of the eastern Paleo-Tethys Ocean br.TECTONOPHYSICS,843,22.
MLA Wang, Yin,et al."Correlation among the Ailaoshan-Song Ma-Song Chay orogenic belts and implications for the evolution of the eastern Paleo-Tethys Ocean br".TECTONOPHYSICS 843(2022):22.
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