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CHEN Guochao, PEI Xianzhi, LI Ruibao, et al. Geological Characteristics and Tectonic Significance of Jurassic Yangqu Formation from Alake Lake Area in the Eastern Part of East Kunlun Orogenic Belt[J]. Northwestern Geology, 2017, 50(3): 113-125.
Citation: CHEN Guochao, PEI Xianzhi, LI Ruibao, et al. Geological Characteristics and Tectonic Significance of Jurassic Yangqu Formation from Alake Lake Area in the Eastern Part of East Kunlun Orogenic Belt[J]. Northwestern Geology, 2017, 50(3): 113-125.
shu

Geological Characteristics and Tectonic Significance of Jurassic Yangqu Formation from Alake Lake Area in the Eastern Part of East Kunlun Orogenic Belt

  • 1. Key Laboratory of Western Mineral Resources and Geological Engineering of Ministry of Education, Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits of Ministry of Land and Resources, School of Earth Science and Resources of Chang'an University, Xi'an 710054, Shaanxi, China;

  • 2. School of Civil Engineeringy, Nanyang Institute of Technology, Nanyang 473000, Henan, China;

  • 3. School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China;

  • 4. Gansu Institute of Geological Survey, Lnazhou 730000, Gansu, China

More Information
  • Received Date: November 08, 2016
  • Revised Date: July 01, 2017
  • Available Online: July 28, 2022
  • Published Date: September 04, 2017
    Graphical Abstract
    • Abstract
  • The early Jurassic Yangqu Formation, newly identified at Alake Lake area during the process of 1:50000 geological mapping in the eastern part of East Kunlun orogenic belt, is observed and depicted carefully both outdoor and indoor in the view of sedimentary faciology, which has been subdivided into 3 lithology beds according to their lithological differences from bottom to top, namely, conglomerate lithology bed (J1y1), sandstone and siltstone lithology bed (J1y2) and rhythmic lithology bed (J1y3). This Formation can be summarized as a stratigraphic sequence of continental faciology with fluvial deposits-lacustrine deposits-fluvial deposits. Based on the regional data, it is supposed that this strata may be the sedimentary response to the strength field transition from compression to extension for the eastern part of East Kunlun orogenic belt during middle Triassic-early Jurassic.
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