中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Synchronous Sedimentation in Gonjo Basin, Southeast Tibet in Response to India-Asia Collision Constrained by Magnetostratigraphy

文献类型:期刊论文

作者Xiao, R.1,2; Zheng, Y.3,4; Liu, X.2; Yang, Q.2; Liu, G.2; Xia, L.2; Bian, Z.2; Guan, J.2; Feng, P.2; Xu, H.2
刊名GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
出版日期2021-03-01
卷号22期号:3页码:22
关键词anisotropy of magnetic susceptibility (AMS) basin evolution Gonjo Basin magnetostratigraphy southeast Tibetan Plateau
DOI10.1029/2020GC009411
通讯作者Zhang, Y.(zhengyan@ivpp.ac.cn) ; Zheng, H.(zhenghb@ynu.edu.cn)
英文摘要The India-Asia collision has been the object of vigorous debate for decades, with ages of the start ranging from Late Cretaceous to Oligocene. Sedimentary records preserved in both near-field and far-field settings provide critical evidence concerning the age and mechanism of the collision. Gonjo Basin, one of a series of fault-controlled basins developed along the eastern margin of Tibetan Plateau, contains well-exposed sedimentary successions, providing great potential for understanding depositional, tectonic-geomorphological and climatic history associated with India-Asia collision and plateau uplift. Lithofacies analysis reveals that the sequences consist of sandstone, mudstone and conglomerate, formed in fluvial-lacustrine systems. High-resolution magnetostratigraphy, constrained by U-Pb dating of zircon from a volcaniclastic layer which has been found in the central Gonjo Basin for the first time, indicates that sedimentation started at 69 Ma and continued in this locality until 50 Ma. Anisotropy of magnetic susceptibility (AMS) interpretation based on the age framework reveals a post-depositional compression after 50 Ma, responding simultaneously to the early uplift of southeast Tibetan Plateau driven by India-Asia collision.
资助项目Second Tibetan Plateau Scientific Expedition and Research (STEP)[2019QZKK0704] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB26020301] ; National Natural Science Foundation of China (NSFC)[41974079] ; National Natural Science Foundation of China (NSFC)[U1902208] ; National Natural Science Foundation of China (NSFC)[41991223] ; National Natural Science Foundation of China (NSFC)[41888101] ; National Natural Science Foundation of China (NSFC)[41991323]
WOS研究方向Geochemistry & Geophysics
语种英语
出版者AMER GEOPHYSICAL UNION
WOS记录号WOS:000636360200009
资助机构Second Tibetan Plateau Scientific Expedition and Research (STEP) ; Strategic Priority Research Program of the Chinese Academy of Sciences ; National Natural Science Foundation of China (NSFC)
源URL[http://ir.ieecas.cn/handle/361006/16274]  
专题地球环境研究所_古环境研究室
通讯作者Zhang, Y.; Zheng, H.
作者单位1.Nanjing Normal Univ, Sch Geog Sci, Nanjing, Peoples R China
2.Yunnan Univ, Yunnan Key Lab Earth Syst Sci, Kunming, Yunnan, Peoples R China
3.Chinese Acad Sci, Key Lab Vertebrate Evolution & Human Origins, Inst Vertebrate Palentol & Paleoanthropol, Beijing, Peoples R China
4.CAS Ctr Excellence Life & Paleoenvironm, Beijing, Peoples R China
5.Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA
6.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian, Peoples R China
7.Univ Queensland, Sch Earth & Environm Sci, Brisbane, Qld, Australia
推荐引用方式
GB/T 7714
Xiao, R.,Zheng, Y.,Liu, X.,et al. Synchronous Sedimentation in Gonjo Basin, Southeast Tibet in Response to India-Asia Collision Constrained by Magnetostratigraphy[J]. GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,2021,22(3):22.
APA Xiao, R..,Zheng, Y..,Liu, X..,Yang, Q..,Liu, G..,...&Zheng, H..(2021).Synchronous Sedimentation in Gonjo Basin, Southeast Tibet in Response to India-Asia Collision Constrained by Magnetostratigraphy.GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,22(3),22.
MLA Xiao, R.,et al."Synchronous Sedimentation in Gonjo Basin, Southeast Tibet in Response to India-Asia Collision Constrained by Magnetostratigraphy".GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS 22.3(2021):22.

入库方式: OAI收割

来源:地球环境研究所

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