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ZHANG Xinquan, ZHANG Zhenli, WANG Jingui, WANG Shuo, YANG Xinpeng, ZHUAN Shaopeng, HOU Dehua, ZHANG Zeguo, ZHANG Liguo, CHENG Zhou. 2020. Further discussion on the formation and evolution of the Yarlung Zangbo suture zone, Tibet[J]. Geology in China, 47(4): 944-970. doi: 10.12029/gc20200404
Citation: ZHANG Xinquan, ZHANG Zhenli, WANG Jingui, WANG Shuo, YANG Xinpeng, ZHUAN Shaopeng, HOU Dehua, ZHANG Zeguo, ZHANG Liguo, CHENG Zhou. 2020. Further discussion on the formation and evolution of the Yarlung Zangbo suture zone, Tibet[J]. Geology in China, 47(4): 944-970. doi: 10.12029/gc20200404
shu

Further discussion on the formation and evolution of the Yarlung Zangbo suture zone, Tibet

  • 1.

    Hebei Regional Geological Survey Institute, Langfang 065000, Hebei, China

  • 2.

    Hebei GEO University, Shijiazhuang 050031, Hebei, China

  • 3.

    No.5 Geological Party, Tibet Bureau of Geology and Mining Exploration and Development, Golmud 816000, Qinghai, China

    • Fund Project: Supported by the project of China Geological Survey(No. DD20160015-09)
More Information
  • Author Bio: ZHANG Xinquan, female, born in 1988, engineer, engages in the study of regional geological and mineral resource survey; E-mail:qdsdksc@163.com
  • Corresponding author: WANG Jingui, male, born in 1986, master, engineer, research direction of geotectonics and tectonic dynamics; E-mail:airstarry@163.com 
Received Date:  24 May 2018
Revised Date:  13 August 2018
Publish Date:  25 August 2020
    Abstract

  • Based on a comprehensive study of 1:50000 regional geological survey and relevant data collection, this paper further discusses the formation and evolution of the Yarluzangbo suture zone. The Tethys Ocean in the Yarlung Zangbo had the nature of the back-arc expanded ocean basin. From Early Triassic to mid Middle Triassic period, the oceanic basin was formed preliminarily, completely formed in late Middle Triassic to Late Triassic period, then gradually shrank from Early Jurassic to Late Cretaceous period, and was finally closed in Paleocene-Eocene period. The ophiolite in the southern belt was mainly of the mid oceanic ridge dilatation type (type MORB) formed in late Middle Triassic to Late Triassic period. The ophiolites in the northern belt seem mainly to have been the upper plate of the subduction zone (type SSZ) related to intra-oceanic subduction, formed in the early Middle Jurassic period. The other Jurassic-Cretaceous magmatic rocks in the belt were mainly fore-arc basalt rocks (type FAB). It is shown that the Tethys Ocean in the Yarlung Zangbo began its intra-oceanic subduction in the Early Jurassic, and synchronously subducted actively northward under the Gangdise belt, subducted passively southward under the Himalaya landmass, and then continued to develop until the Late Cretaceous. The Palaeocene-Eocene subduction and collision and extinction were transformed into a binding zone.

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