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YUAN Sihua, LIU Yongjiang, CHANG Ruihong, NEUBAUER Franz, GENSER Johann, GUAN Qingbing, HUANG Qianwen. 2021. A brief review on the tectonic evolution of the west Tethysides. Sedimentary Geology and Tethyan Geology, 41(2): 316-331. doi: 10.19826/j.cnki.1009-3850.2021.02004
Citation: YUAN Sihua, LIU Yongjiang, CHANG Ruihong, NEUBAUER Franz, GENSER Johann, GUAN Qingbing, HUANG Qianwen. 2021. A brief review on the tectonic evolution of the west Tethysides. Sedimentary Geology and Tethyan Geology, 41(2): 316-331. doi: 10.19826/j.cnki.1009-3850.2021.02004
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A brief review on the tectonic evolution of the west Tethysides

  • 1. College of Earth Sciences, Institute of Disaster Prevention, Sanhe 065201, Hebei, China;

  • 2. Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE, College of Marine Geosciences, Ocean University of China, Qingdao 266100, Shandong, China;

  • 3. Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, Shandong, China;

  • 4. Paris-Lodron-University of Salzburg, Department of Geography and Geology, Geology Division, Hellbrunnerstraβe 34, 5020 Salzburg, Austria;

  • 5. Hebei Key Laboratory of Earthquake Dynamics, Sanhe 065201, Hebei, China

Received Date:  02 January 2020
Revised Date:  05 February 2020
    Abstract
  • The research progress of the main suture zones in the west Tethysides and the development characteristics of the oceanic basin represented by them are reviewed. We propose the potential location of the Paleo-Tethys suture and summarize a brief evolution of the Paleo-Tethyan Ocean. Combining with regional geological data, this paper discusses the tectonic framework of the west Tethysides during the latest Paleozoic to the Mesozoic. The similar tectonic evolution is also found within the Paleo-Tethys which can be compared between the east and west parts. From the latest Paleozoic onward, the west Tethysides realm was mainly affected by double-sided subduction of the Paleo-Tethys.The Neo-Tethys was characterised by archipelagic arc-basin system during the Mesozoic, which succeed the Permian rifts in the aftermath of the Paleo-Tethys subduction. The west Tethysides was mainly manifested by the orogenesis of collaped back-arc basin.
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