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    XIE Chaoming, LI Cai, LI Guangming, WANG Bin, DONG Yuchao, HAO Yujie, . The research progress and problem of the Sumdo Paleo-Tethys Ocean, Tibet[J]. Sedimentary Geology and Tethyan Geology, 2020, 40(2): 1-13. DOI: 10.19826/j.cnki.1009-3850.(2020)02-0001-13
    Citation: XIE Chaoming, LI Cai, LI Guangming, WANG Bin, DONG Yuchao, HAO Yujie, . The research progress and problem of the Sumdo Paleo-Tethys Ocean, Tibet[J]. Sedimentary Geology and Tethyan Geology, 2020, 40(2): 1-13. DOI: 10.19826/j.cnki.1009-3850.(2020)02-0001-13
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    The research progress and problem of the Sumdo Paleo-Tethys Ocean, Tibet

    • 1. College of Earth Science, Jilin University, Changchun, 130061, Jilin, China;

    • 2. Research Center for Tibetan Plateau, Jilin University, Changchun, 130061, Jilin, China;

    • 3. Chengdu Center, China Geological Survey, Chengdu 610081, Sichuan, China;

    • 4. Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources of China, Changchun 130061, Jilin, China

    More Information
    • Received Date: April 09, 2020
    • Revised Date: May 09, 2020
    • Published Date: June 29, 2020
      Graphical Abstract
      • Abstract
    • The evolution process of the Paleo-Tethys tectonic domain on the Qinghai-Tibet plateau has always been a frontier and hotspot of geological research. In order to better understand the tectonic evolution history of the Paleo-Tethys ocean on the Qinghai-Tibet plateau, based on the previous studies, this paper systematically summarized the latest research progress made in recent years in the 1:50,000 regional geological survey, and preliminarily discussed the material composition and the age of subduction and actinic complex zone in the Tangjia-Sundo area. The results show that relatively complete mélange closely related to the evolution of the Paleo-Tethys ocean and the transition of ocean and land are preserved in the Tangjia-Sumdo area in central Gangdise, Tibet, which is an ideal target area for recovery and inversion of the evolution of the Paleo-Tethys ocean. The geological records of the Sumdo Paleo-Tethys crust and its extinction mainly include the late Paleozoic Tangjia-Sumdo ophiolite mélange belt, middle Permian ocean island fragments, high pressure metamorphic belt, late Triassic-early Jurassic magmatism and late Triassic-early Jurassic molassite formation. On the basis of the above work, the evolution process of the Sumdo Paleo-Tethys is preliminarily discussed. These geological records are of great significance to the recovery and inversion of the Paleo-Tethys tectonic evolution on the Qinghai-Tibet plateau.
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      • References (94)
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