中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Indo-Burma passive amalgamation along the Kaladan Fault: Insights from zircon provenance in the Chittagong-Tripura Fold Belt (Bangladesh)

文献类型:期刊论文

作者Yang, Lei4,5; Xiao, Wenjiao3,4; Rahman, M. Julleh Jalalur2; Windley, Brian F.1; Schulmann, Karel6; Ao, Songjian4; Zhang, Ji'en4; Chen, Zhenyu4; Hossain, Md Sakawat2; Dong, Yunpeng5
刊名GEOLOGICAL SOCIETY OF AMERICA BULLETIN
出版日期2020-09-01
卷号132期号:9-10页码:1953-1968
ISSN号0016-7606
DOI10.1130/B35429.1
英文摘要A clear insight of the Indo-Burma amalgamation is required for an understanding of the complex processes of the Indo-Asian collision. Where and when the northeastern part of the Indian subcontinent amalgamated with the Burma plate has not yet been well defined. In order to better understand the tectonic affiliations and evolution of the Indo-Burma Ranges (IBR), we report new detrital zircon U-Pb and Hf isotope data of nine sandstone/siltstone samples (late Miocene- Pliocene) from the Chittagong-Tripura Fold Belt, Bangladesh, which is in the Neogene belt of the IBR. Our results show that the zircon ages of all nine samples have three peaks at <200 Ma, ca. 500 Ma, and 800-1000 Ma. The percentage of young (<200 Ma) zircons increase from the Boka Bil Formation (6.9% to 15.2%) to the Tipam Formation (20.3% to 27.6%). The epsilon(Hf)(t) of most young zircons from the Boka Bil Formation suggest derivation from the Gangdese arc, whereas those from the Tipam Formation show an affinity with the Burma magmatic arc. Therefore, we suggest that the increase of young zircons in the Tipam Formation came from the Burma plate. Comparing provenances of the Paleogene and Neogene belts of the IBR, we suggest that they belong to the Burma plate and Indian subcontinent, respectively, and that the Kaladan Fault, separating these two belts, is the suture between the Indian and Burma terranes. The time of amalgamation is constrained by the ca. 2.5-3.9 Ma boundary between the Boka Bil and Tipam formations, and the eastern Indian promontory likely collided with the Burma plate ca. 11-12 Ma.
WOS关键词PB GEOCHRONOLOGICAL EVIDENCE ; EARLY PALEOZOIC TECTONISM ; HF ISOTOPIC CONSTRAINTS ; MOGOK METAMORPHIC BELT ; MYANMAR OROGENIC BELT ; ASIA COLLISION ONSET ; U-PB ; BENGAL BASIN ; FORE-ARC ; OPHIOLITE COMPLEX
资助项目Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS)[XDB18020203] ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS)[XDB03010801] ; Key Research Program of Frontier Sciences, CAS[QYZDJ-SSWSYS012] ; National Natural Science Foundation of China[41230207] ; National Natural Science Foundation of China[41202150]
WOS研究方向Geology
语种英语
WOS记录号WOS:000565754100010
出版者GEOLOGICAL SOC AMER, INC
资助机构Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences (CAS) ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/97790]  
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Xiao, Wenjiao
作者单位1.Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England
2.Jahangirnagar Univ, Dept Geol Sci, Dhaka 1342, Bangladesh
3.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
5.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian, Peoples R China
6.Univ Strasbourg, Inst Phys Globe Strasbourg, UMR 7516, CNRS,Ecole & Observ Sci Terre, Strasbourg, France
推荐引用方式
GB/T 7714
Yang, Lei,Xiao, Wenjiao,Rahman, M. Julleh Jalalur,et al. Indo-Burma passive amalgamation along the Kaladan Fault: Insights from zircon provenance in the Chittagong-Tripura Fold Belt (Bangladesh)[J]. GEOLOGICAL SOCIETY OF AMERICA BULLETIN,2020,132(9-10):1953-1968.
APA Yang, Lei.,Xiao, Wenjiao.,Rahman, M. Julleh Jalalur.,Windley, Brian F..,Schulmann, Karel.,...&Dong, Yunpeng.(2020).Indo-Burma passive amalgamation along the Kaladan Fault: Insights from zircon provenance in the Chittagong-Tripura Fold Belt (Bangladesh).GEOLOGICAL SOCIETY OF AMERICA BULLETIN,132(9-10),1953-1968.
MLA Yang, Lei,et al."Indo-Burma passive amalgamation along the Kaladan Fault: Insights from zircon provenance in the Chittagong-Tripura Fold Belt (Bangladesh)".GEOLOGICAL SOCIETY OF AMERICA BULLETIN 132.9-10(2020):1953-1968.

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来源:地质与地球物理研究所

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