Geochemistry of Eocene to Pliocene strata of the Bengal Basin: Implications for provenance and erosion of the Himalaya
文献类型：期刊论文
| 作者 | Yang, Lei3,4; Xiao, Wenjiao2,3; Rahman, M. Julleh Jalalur1; Dong, Yunpeng4; Ao, Songjian3; Sun, Jiaopeng4; Chen, Zhenyu3 |
| 刊名 | GEOLOGICAL JOURNAL
 |
| 出版日期 | 2020-10-29 |
| 页码 | 17 |
| ISSN号 | 0072-1050 |
| 关键词 | Bengal Basin erosion of the Himalaya geochemistry provenance sedimentary rock |
| DOI | 10.1002/gj.4025 |
| 英文摘要 | The earliest record of Himalayan detritus in the Himalayan foreland and the erosion sequence of different lithotectonic units of the Himalaya are critical for reconstructing collision and crustal deformation of the orogenic belt. In this study, bulk-rock major, trace and rare earth elements of 19 fine-grained clastic sedimentary rock samples from Eocene to Pliocene strata of the Bengal Basin were examined to study their provenance and erosion of the Himalaya. Combining with previous detrital zircon age data from the Bengal Basin, Nepal foreland basin, and South Tibet, we suggest that detritus from the uplifted Tethyan Himalayan Sequences and the Gangdese Arc had not been carried into the Himalayan foreland at least before Late Miocene, and that the Bengal Basin was in a passive continental margin setting from Eocene to Early Miocene, receiving detritus from a felsic sedimentary rock source. The earliest Himalayan detritus recorded in the Eocene strata of Bengal Basin were probably derived from the antecedent sedimentary cover of the Greater Himalayan crystalline rocks. We assume that the lack of Cretaceous Gangdese detritus in the Himalayan foreland from Eocene to Middle Miocene is due to a geomorphic barrier between the Tethyan Himalaya and the Himalayan foreland. Detritus from the Greater Himalayan crystalline rocks were first recorded in the Middle-Late Miocene Boka Bil Formation of the Bengal Basin, which is consistent with the uplift and exhumation time of the Greater Himalayan Sequences. |
| WOS关键词 | ZIRCON U-PB ; SANDSTONE DETRITAL MODES ; HF ISOTOPIC CONSTRAINTS ; WHOLE-ROCK GEOCHEMISTRY ; NEOGENE SURMA GROUP ; SEDIMENTARY-ROCKS ; SOUTHERN TIBET ; FOLD BELT ; TECTONOMETAMORPHIC DISCONTINUITIES ; REE GEOCHEMISTRY |
| 资助项目 | MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; Key Research Program of Frontier Sciences, CAS[QYZDJ-SSW-SYS012] ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences[XDB03010801] ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences[XDB18020203] |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| 出版者 | WILEY |
| WOS记录号 | WOS:000583528500001 |
| 资助机构 | MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; 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 ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; 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 ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; 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 ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University ; 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 ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/98702]  |
| 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 | Yang, Lei |
| 作者单位 | 1.Jahangirnagar Univ, Dept Geol Sci, Dhaka, Bangladesh 2.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China 4.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian, Peoples R China |
| 推荐引用方式 GB/T 7714 | Yang, Lei,Xiao, Wenjiao,Rahman, M. Julleh Jalalur,et al. Geochemistry of Eocene to Pliocene strata of the Bengal Basin: Implications for provenance and erosion of the Himalaya[J]. GEOLOGICAL JOURNAL,2020:17. |
| APA | Yang, Lei.,Xiao, Wenjiao.,Rahman, M. Julleh Jalalur.,Dong, Yunpeng.,Ao, Songjian.,...&Chen, Zhenyu.(2020).Geochemistry of Eocene to Pliocene strata of the Bengal Basin: Implications for provenance and erosion of the Himalaya.GEOLOGICAL JOURNAL,17. |
| MLA | Yang, Lei,et al."Geochemistry of Eocene to Pliocene strata of the Bengal Basin: Implications for provenance and erosion of the Himalaya".GEOLOGICAL JOURNAL (2020):17. |
入库方式： OAI收割
来源：地质与地球物理研究所
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