Lithologic Reservoirs ›› 2021, Vol. 33 ›› Issue (2): 26-35.doi: 10.12108/yxyqc.20210204

• PETROLEUM GEOLOGY • Previous Articles     Next Articles

Characteristics of breccia reservoir of Tuylock Formation of well Beixin-1 in Markit Slope of Tarim Basin

LI Huili1, YOU Donghua2, LI Jianjiao1, TAN Guanghui3, LIU Shilin4   

  1. 1. Research Institute of Petroleum Exploration & Production, Sinopec, Beijing 100083, China;
    2. Wuxi Research Institute of Petroleum Geology, Research Institute of Petroleum Exploration & Production, Sinopec, Wuxi 214126, Jiangsu, China;
    3. Research Institute of Exploration and Development, Sinopec Northwest Oilfield Company, Urumqi 830011, China;
    4. Department of Oilfield Exploration & Development, Sinopec, Beijing 100728, China
  • Received:2020-09-06 Revised:2020-10-13 Online:2021-04-01 Published:2021-03-31

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Abstract: A set of dolomite and dolomitic breccia reservoir covered by the gypsum bed of Aertashi Formation was firstly drilled in well Beixin-1 in Markit Slope of Tarim Basin,which obtained oil and gas discovery. In order to define reservoir characteristics,studies on reservoir physical properties,reservoir space,diagenesis and genesis were carried out by using the data obtained from continuous coring of the test production section. The results show that the dolomitic breccia reservoir has good reservoir physical properties,and fractures, dissolved pores and cavities are the main types of reservoir space,which mainly distributed in the brecciated silty dolomites and silty dolomites. The gypsum dissolution in the para-syngenetic period and early diagenetic stage and the tectonic rupture in Himalayan tectonic movement are the mainly constructive diagenesis. The original sedimentary environment of dolomitic breccia was limited tidal flat or lagoon, and the reservoir was developed by gypsum dissolution,and reformed by tectonic rupture during the Himalayan period.

Key words: reservoir characteristics, breccia reservoir, gypsum dissolution, tectonic rupture, Tuylock Formation, Markit Slope, Tarim Basin

CLC Number: 

  • TE122.2
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