Tectonic Subsidence of Yining Depression and Its Main Controlling Factors
 
 

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  • 1.Postdoctoral Research institute Henan Oilfield Company Sinopec,Nanyang 473000,China;
    2.Key Laboratory of Petroleum Resources Research,Institute of Geology and Geophysics,Chinese Academy ofSciences,Lanzhou 730000,
    China;3.Reasearch institute Exploration and Development Henan Oilfield Company,SINOPEC,Zhengzhou 450016,China

Received date: 2013-11-22

  Revised date: 2014-01-08

  Online published: 2014-08-10

Abstract

The Late Jurassic stratigraphic erosion has been estimated according to the data of several drilling wells,simulation wells and seismic data in the Yining Sag.The results show that the structure history of Yining Depression contains three rapid subsidence periods,two slow subsidence periods and two regional rapid uplifting periods since the Middle Permian.The largest subsidence time was in the Middle Permian-Early Triassic Period which was caused by thermal subsidence after Hercynian Volcanic Rifts and the subsidence center was located in Huocheng area of central depression.Rapid subsidence period in Early Jurassic and after Nelgene was less significant,different lifting regularity which was caused by tectonic movement is the main reason for these two rapid subsidence periods.With an obvious east-west difference,Late Jurassic-Early Cretaceous was the major uplift and erosion period,and the eroded intensity of west is much greater than that in the eastern region.
 

Cite this article

ZHU Jian-jun,LIN Shui-qing,ZHANG Hong-jun,ZHANG Gao-yuan,YING Wen-xi,GU Chao,WANG Qi2 .

Tectonic Subsidence of Yining Depression and Its Main Controlling Factors
 
 
[J]. Natural Gas Geoscience, 2014 , 25(8) : 1181 -1187 . DOI: 10.11764/j.issn.1672-1926.2014.08.1181

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