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YANG Wei, TIAN Jing-chun, ZHU Ying-tang, WANG Feng. The storm deposits in the Upper Permian Shiqianfeng Formation in the Dengfeng region,Henan[J]. Sedimentary Geology and Tethyan Geology, 2009, 29(1): 65-70.
Citation: YANG Wei, TIAN Jing-chun, ZHU Ying-tang, WANG Feng. The storm deposits in the Upper Permian Shiqianfeng Formation in the Dengfeng region,Henan[J]. Sedimentary Geology and Tethyan Geology, 2009, 29(1): 65-70.
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The storm deposits in the Upper Permian Shiqianfeng Formation in the Dengfeng region,Henan

  • 1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China;

  • 2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, Sichuan, China;

  • 3. College of Information Engineering, Chengdu University of Technology, Chengdu 610059, Sichuan, China

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  • Published Date: March 29, 2009
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    • Abstract
  • The Upper Permian Shiqianfeng Formation in the Dengfeng region,Henan is mainly composed of the lacustrine clastic rocks in which the tempestites are well developed.These tempestites have the features of sedimentary structures including scour surface,hummocky cross-beddings,convolute beddings,ripple beddings and water-escape structures.The idealized sedimentary sequences of the tempestites are generalized and consist,from bottom to top,of the intervals Sa,Sb,Sc,Sd and Se.The types of the tempestites include autochthonous and allochthonous tempestites,indicating a typical lacustrine environment.The identification of the tempestites in the study area has an important significance for the recognition of sedimentary facies and reconstruction of the palaeogeographic environments of the Upper Permian Shiqianfeng Formation in the Dengfeng region,Henan.
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