Opening of the Neo-Tethys Ocean in the Late Triassic? Sedimentary responses on the northern Indian continental margin

被引:0
|
作者
Meng Z. [1 ,2 ]
Wang J. [1 ]
Li W. [1 ,3 ]
机构
[1] Slate Key Laboratory of Lithosphere Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing
[2] Tianjin Center, China Geological Survey North China Center for Geoscience Innovation, Tianjin
[3] College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing
来源
Dizhi Xuebao/Acta Geologica Sinica | 2023年 / 97卷 / 09期
关键词
Late Triassic; northern Indian continental margin; opening of Neo-Tethys; paleogcography; sedimentary response; Tethyan Himalaya;
D O I
10.19762/j.cnki.dizhixuebao.2023155
中图分类号
学科分类号
摘要
The Neo-Tethys recorded by the Indus-Yarlung-Zangbo suture zone in southern Tibet was a vast ocean between Eurasian and Gondwanan continents during the Mesozoic that closed in southern Tibet as a result of Indo-Eurasian collision in the Early Cenozoic. It is a common view that the Neo-Tethys Ocean was formed as a result of rifting of the Lhasa block from the Eastern Gondwana. However, the timing of the rift remains controversial. Proposed timings for the opening of the Neo-Tethys vary from Early Permian to Late Triassic. In this study, we carried out an integrated stratigraphic and sedimentological study on the Permian-Triassic strata deposited on the north Indian continental margin. Our data indicated that the depositional environment remained stable since cessation of the glacial period in the Early Permian. A notable change in sedimentary environment occurred only in the Late Triassic, from a carbonate platform to a terrigenous clastic shelf. Facies change was accompanied by increasing depositional rate, accelerating tectonic subsidence, provenance change, bimodal volcanism, and paleogcographic reconstruction. These changes clearly revealed a regional extensional event, which is considered as a response to the opening of Neo-Tethys. © 2023 Geological Society of China. All rights reserved.
引用
收藏
页码:3024 / 3042
页数:18
相关论文
共 88 条
  • [1] Briihwiler T, Bucher H, Goudemand N., Smithian (Early Triassic) ammonoids from Tulong, South Tibet, Geobios, 43, pp. 403-431, (2009)
  • [2] Cai Fulong, Ding Lin, Laskowski A K, Kapp P, Wang Houqi, Xu Qiang, Late Triassic paleogeographic reconstruction along the Neo-Tethyan Ocean margins, southern Tibet, Earth Planetary Science Letters, 435, pp. 105-114, (2016)
  • [3] Cao Huawen, Huang Yong, Li Guangming, Zhang Linkui, Wu Jianyang, Dong Lei, Dai Zuowen, Liu Lu, Late Triassic sedimentary records in the northern Tethyan Himalaya: Tectonic link with greater India, Geoscience Frontiers, 9, pp. 273-291, (2018)
  • [4] Dishu Chen, Hui Luo, Xueheng Wang, Bo Xu, Matsuoka A., Late Anisian radiolarian assemblages from the Yarlung-Tsangpo Suture Zone in the Jinlu area, Zedong, southern Tibet: Implications for the evolution of Neotethys, Island Arc, 28, (2019)
  • [5] Chen Jinhua, Yang Shengqiu, Eleganuculana, new genus, and some other bivalves from the upper Triassic of Kangmar in Xizang, Acta Palaeontologica Sinca, 22, 3, pp. 355-358, (1983)
  • [6] Chen Junbing, Xu Xingyong, Li Wenqing, Gongbu, New advances in research of Permian-Carboniferous in the Kangmar region, southern Tibet, Geoscience, 16, 3, pp. 237-242, (2002)
  • [7] Jingen Dai, Chengshan Wang, Hebert R, Yalin Li, Hanting Zhong, Guillaume R, Bezard R, Wei Yushuai, Late Devonian OIB alkaline gabbro in the Yarlung Zangbo suture zone: Remnants of the Paleo-Tethys?, Gondwana Research, 19, pp. 232-243, (2011)
  • [8] Dumont T, Ro&die
  • [9] Hl U., Tectonics and sea-level changes recorded in Late Triassic sequences at rifted margins of eastern and western Tethys (Northwest Australia, Leg 122, Western Europe), Washington DC American Geophysical Union Geophysical Monograph Series, 70, pp. 185-202, (1992)
  • [10] Exon N F, Buffler R T., Mesozoic seismic stratigraphy and tectonic evolution of the western Exmouth Plateau, Proceedings of the Ocean Drilling Program, Scientific Results, 122, pp. 61-81, (1992)