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Geochemistry and detrital zircon U-Pb dating of Pliocene-Pleistocene sandstones of the Chittagong Tripura Fold Belt (Bangladesh): Implications for provenance
Rahman, M. Julleh Jalalur1; Xiao, Wenjiao2,3; Hossain, Md Sakawat1; Yeasmin, Rumana1; Sayem, Abu Sadat Md1; Ao, Songjian2; Yang, Lei2; Abdullah, Rashed1; Dina, Nafisa Tamanaya4
2020-02-01
Source PublicationGONDWANA RESEARCH
ISSN1342-937X
Volume78Pages:278-290
AbstractThe Bengal Basin originated during the collision of India with Eurasia and Burma. The provenance analysis of the Chittagong Tripura Fold Belt (CTFB), which is the folded eastern flank of the Bengal Basin as well as the Neogene belt of the Indo-Burman Ranges (IBR) is key to better understand the possible sources of sediment input from the complex interplay of the Indian, Eurasian and Burma plates. We report new whole rock geochemical and detrital zircon U-Pb data from the upper Neogene sandstones of Tipam-Dupi Tila formations (Pliocene to Plio-Plestocene succession) from the CTFB. Detrital zircon U-Pb age spectra show three predominant peaks at <200 Ma, 480-650, similar to 800-1000 Ma. The geochemical discriminations and elemental ratios of Eu/Eu* (similar to 0.70), La/Sc (similar to 16.13), La/Co (similar to 15.76), Th/Sc (similar to 2.95), La/Th (similar to 5.67), Th/Co (similar to 2.87), Cr/Th (similar to 4.63) as well as Chondrite-normalized REE patterns with flat HREE, LREE enrichment, and negative Eu anomalies for the Tipam and Dupi Tila formations are suggestive of a dominantly felsic source area experiencing moderate to intensive chemical weathering (Chemical index of alteration, CIA - 57 to 81) and have a recycled provenance orogen related to active continental or passive margin settings. Integrated geochemical and zircon UePb studies reveal that the main sediment input might have been from the Himalayan orogen with significant arc-derived detritus, possibly from the Gangdese arc as well as from the Burma magmatic arc. (c) 2019 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
KeywordGeochemistry U-Pb dating Pliocene-Pleistocene sandstones Provenance Bengal Basin
DOI10.1016/j.gr.2019.07.018
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 ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, 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 ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, 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 ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, 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 ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China
WOS KeywordPENNSYLVANIAN-PERMIAN AGE ; TECTONIC SETTING DISCRIMINATION ; WHOLE-ROCK GEOCHEMISTRY ; NEOGENE SURMA GROUP ; BENGAL BASIN ; SEDIMENTARY-ROCKS ; SYLHET TROUGH ; ISOTOPIC COMPOSITION ; CRUSTAL EVOLUTION ; TRACE
Language英语
Funding ProjectNational Natural Science Foundation of China[41888101] ; National Natural Science Foundation of China[41202150] ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China[XDB18020203] ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China[XDB03010801] ; Key Research Program of Frontier Sciences, CAS, China[QYZDJ-SSW-SYS012]
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 ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, 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 ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, 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 ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, 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 ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China ; Key Research Program of Frontier Sciences, CAS, China
WOS Research AreaGeology
WOS SubjectGeosciences, Multidisciplinary
WOS IDWOS:000522973500016
PublisherELSEVIER
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/95503
Collection岩石圈演化国家重点实验室
Corresponding AuthorRahman, M. Julleh Jalalur; Xiao, Wenjiao
Affiliation1.Jahangirnagar Univ, Dept Geol Sci, Dhaka 1342, Bangladesh
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
4.Bangladesh Atom Energy Commiss, Dhaka 1342, Bangladesh
Corresponding Author AffilicationInstitute of Geology and Geophysics, Chinese Academy of Sciences
Recommended Citation
GB/T 7714
Rahman, M. Julleh Jalalur,Xiao, Wenjiao,Hossain, Md Sakawat,et al. Geochemistry and detrital zircon U-Pb dating of Pliocene-Pleistocene sandstones of the Chittagong Tripura Fold Belt (Bangladesh): Implications for provenance[J]. GONDWANA RESEARCH,2020,78:278-290.
APA Rahman, M. Julleh Jalalur.,Xiao, Wenjiao.,Hossain, Md Sakawat.,Yeasmin, Rumana.,Sayem, Abu Sadat Md.,...&Dina, Nafisa Tamanaya.(2020).Geochemistry and detrital zircon U-Pb dating of Pliocene-Pleistocene sandstones of the Chittagong Tripura Fold Belt (Bangladesh): Implications for provenance.GONDWANA RESEARCH,78,278-290.
MLA Rahman, M. Julleh Jalalur,et al."Geochemistry and detrital zircon U-Pb dating of Pliocene-Pleistocene sandstones of the Chittagong Tripura Fold Belt (Bangladesh): Implications for provenance".GONDWANA RESEARCH 78(2020):278-290.
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