THE GEOLOGY FEATURE of DINA 2 GAS FIELD,KUCHE DEPRESSION

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  • 1.Branch of Tarim Oilfield Company,CNPC,Kuerle 841000,China;2.University of Petroleum,Beijing 102249, China

Received date: 2003-04-28

  Revised date: 2003-08-12

  Online published: 2003-10-20

Abstract

Dina 2 gas field is situated on the eastern side of Qiulitage structure belt,Kuche depression. It is one of the local structure under the plastic deformation layer salt-section of Jidike formation,Neogene. Paleogene sand is the major bearing gas layer.The content of CH4in natural gas is about 86.7%~88.9%. It's wet gas.Organic geochemical research proved that gas source is mainly from Jurasic coal-bearing series.The rudiment of Dina 2 structure came up into being in Kuche period, late Tertiary, and the structure stopped in Quaternary. It's late accumulation.The large thickness saline rock,gypsite and mudstone of Jidike formation, Quaternary,is the territorial capping bed.The territorial capping bed and late accumulation are the key reasion of the preservation of Dina2  gas field.The abnormal high pressure is caused by the strongly structural compression from the north side began in Pleistocene. Geological reserves of Dina 2 gas field proved and controlled is more than 100 billion cubic metre.

Cite this article

MA Yu-jie,XIE Hui-wen, CAI Zhen-zhong,ZHANG Li-juan,GAO Guo-xi . THE GEOLOGY FEATURE of DINA 2 GAS FIELD,KUCHE DEPRESSION[J]. Natural Gas Geoscience, 2003 , 14(5) : 371 -374 . DOI: 10.11764/j.issn.1672-1926.2003.05.371

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