Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (4): 1002-1010.doi: 10.13278/j.cnki.jjuese.201504104

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Main Controlling Factors of High Quality Deep-Water Mass Transport Deposits (MTDs) Reservoir in Lacustrine Basin:An Insight of Qingshankou Formation, Yingtai Area, Songliao Basin, Northeast China

Chen Bintao1,2, Pan Shuxin1,2, Liang Sujuan1, Zhang Qingshi3, Liu Caiyan1, Wang Ge3   

  1. 1. Research Institute of Petroleum Exploration & Development-Northwest (NWGI), Petrochina, Lanzhou 730020, China;
    2. Key Laboratory of Reservoir Description, CNPC, Lanzhou 730020, China;
    3. Research Institute of Exploration and Development of Daqing Oilfield Company, Daqing 163000, Heilongjiang, China
  • Received:2014-10-02 Published:2015-07-26

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Abstract:

Deepwater sandstone, viewed as poor reservoir traditionally, is now the potential target for increasing reserves and production. However, the exploration practice in recent years showed that deepwater mass transport deposits (MTDs) in lacustrine basin can form high-quality reservoir. Its reservoir properties are even superior to a delta front. Based on the data of core observation, casting thin sections, scanning electron microscope, measured porosity, organic acid content of formation water, and formation overpressure, the main controlling factors of high quality deep-water MTDs in Qingshankou Formation, Yingtai area, Songliao basin have been analyzed. According to the analysis, it can be concluded that MTDs sandstone of Qingshankou Formation is debris-feldspar sandstone with high texture maturity, where the reservoir space is dominated by primary intergranular pores and secondary dissolution pores, and the detrital grains are dominated by point-contacted with low calcite cement and quartz overgrown. The development of a good deepwater sandstone reservoir is controlled by sedimentary process and overpressure cycles. Sedimentary process of MTDs is the foundation, which makes the deepwater sandstone inherit the primary characteristics of porosity and permeability of sandstone in delta front (deposited in high energy environment). Inhibition of destructive diagenesis caused by overpressure is the core factor, which can preserve the primary pores and lead to a low content of cement. Organic acid dissolution can be a supplement to promote the development of secondary pores. MTDs deepwater sandstone of Qingshankou Formation is distributed inside the source rock as lenticulars with good physical properties, which can be treated as favorable exploration targets.

Key words: Songliao basin, mass transport deposits(MTDs), reservoir properties, secondary porosity, overpressure, Qingshankou Formation

CLC Number: 

  • TE122

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