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DONG Li-yang, WANG Jian, YIN Fu-guang, WANG Peng, ZHOU Ye-xin. The storm deposits from the Middle Triassic Beiya Formation in the Beiya region, western Yunnan and their palaeogeographic implications[J]. Sedimentary Geology and Tethyan Geology, 2013, 33(4): 6-15.
Citation: DONG Li-yang, WANG Jian, YIN Fu-guang, WANG Peng, ZHOU Ye-xin. The storm deposits from the Middle Triassic Beiya Formation in the Beiya region, western Yunnan and their palaeogeographic implications[J]. Sedimentary Geology and Tethyan Geology, 2013, 33(4): 6-15.
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The storm deposits from the Middle Triassic Beiya Formation in the Beiya region, western Yunnan and their palaeogeographic implications

  • 1. Chinese Academy of Geological Sciences, Beijing 100037, China;

  • 2. Chengdu Institute of Geology and Mineral Resources, Chengdu 610081, Sichuan, China;

  • 3. College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, Sichuan, China

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  • Received Date: August 04, 2013
  • Published Date: December 29, 2013
    Graphical Abstract
    • Abstract
  • The storm deposits are recognized for the first time from the Middle Triassic Beiya Formation in the Beiya region, western Yunnan, and consist of alternating gravelly limestones and reticulated limestones with abundant sedimentary structures of storm deposits such as erosional soles, lag deposits, graded beddings and hummocky cross-beddings. The background deposits of the storm deposits are dominated by thin-bedded reticulated limestones with wavy beddings and bird's-eye structures, suggesting a tidal-flat environment in the study area. The discovery of the tidal-flat storm deposits may be important to the research of the palaeogeography and palaeoclimatology in the study area during the Middle Triassic.
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