Lithologic Reservoirs ›› 2017, Vol. 29 ›› Issue (5): 67-75.doi: 10.3969/j.issn.1673-8926.2017.05.008

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Characteristics and distribution of Lower-Middle Ordovician grain bank in mid-eastern Tarim Basin

JIANG Haijian1, CHEN Qianglu1, QIAO Guilin1, CAO Zicheng2, CHU Chenglin1   

  1. 1. Wuxi Institute of Petroleum Geology, Research Institute of Petroleum Exploration & Production, Sinopec, Wuxi 214151, Jiangsu, China;
    2. Research Institute of Exploration & Production, Sinopec Northwest Oilfield Company, Urumqi 830011, China
  • Received:2016-12-10 Revised:2017-03-03 Online:2017-09-21 Published:2017-09-21

Abstract: There are several new gas discoveries in Shuntuoguole area of mid-eastern Tarim Basin in recent years. So,it is necessary to re-understanding Lower-Middle Ordovician carbonate sedimentary facies for further exploration. Based on cores,thin sections,logging and seismic data,the characteristics,evolution and distribution of Lower-Middle Ordovician carbonate sedimentary facies were analyzed. Grain bank developed in variety of facies such as low-energy grain bank in the restricted platform,middle to high-energy grain bank facies and middle to lowenergy grain bank facies in open platform,bank facies and reef facies on margin of platform. In Yingshan period, grain bank facies widely developed in gentle slope and low-lying zone of intraplatform in Shuntuoguole area, which open platform grain bank increased local strata thickness. With rapid uprising of sea level,In Yijianfang period,open platform extended to whole Shuntuoguole area,grain bank migrated to Gucheng area and northern Shuntuoguole area. Platform is the key factor to develop grain bank,and the sea level change controls the process and pattern of grain bank.

Key words: alluvial fan, fluvial fan, fluvial deposits, distributive fluvial system, sedimentary system

CLC Number: 

  • TE112.2
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