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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 1993  >  15(3): 252-261
Zhu Hongfa, Qin Deyu, Chen Yue, Wang Shuyi, Wang Genhua. SEDIMENTARY EVOLUTION AND STRUCTURAL BACKGROUND OF THE PERMIAN SYSTEM ON THE BOUNDARY OF JIANGSU—ZHEJIANG—ANHUI PROVINCES[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1993, 15(3): 252-261. doi: 10.11781/sysydz199303252
Citation: Zhu Hongfa, Qin Deyu, Chen Yue, Wang Shuyi, Wang Genhua. SEDIMENTARY EVOLUTION AND STRUCTURAL BACKGROUND OF THE PERMIAN SYSTEM ON THE BOUNDARY OF JIANGSU—ZHEJIANG—ANHUI PROVINCES[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1993, 15(3): 252-261. doi: 10.11781/sysydz199303252
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SEDIMENTARY EVOLUTION AND STRUCTURAL BACKGROUND OF THE PERMIAN SYSTEM ON THE BOUNDARY OF JIANGSU—ZHEJIANG—ANHUI PROVINCES

doi: 10.11781/sysydz199303252

  • Central Lab. of Petroleum Geology, MGMR

  • Received Date: 1991-04-04
  • Publish Date: 1993-07-25
    Abstract
  • The paper discusses the lateral and vertical sedimentary features of the Pemian System developed during the stages of Qixia,Maokou and Changxing on the boundary of Jiangsu-Zhejiang-Anhui province. It is suggested that a series of sedimentary-structural models with regularity of successive extensionally faulted troughs occurred in the Permian System of the region due to the expansion of Paleo-Tethys sea and the extension undergone in the interior continental crust.

     

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