Lithologic Reservoirs ›› 2017, Vol. 29 ›› Issue (2): 87-98.doi: 10.3969/j.issn.1673-8926.2017.02.011

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Characteristics of dolomitic reservoirs of A'ershan Formation in Bayindulan Sag,Erlian Basin

SUN Shuyang1,2, ZHU Xiaomin1,2, WEI Wei1,2, ZHU Shifa1,2, HE Mingwei1,2, LIU Wei1,2, WU Jianping3   

  1. 1. College of Geoscience, China University of Petroleum(Beijing), Beijing 102249, China;
    2. State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum(Beijing), Beijing 102249, China;
    3. Research Institute of Exploration and Development, PetroChina Huabei Oilfield Company, Renqiu 062552, Hebei, China
  • Received:2016-12-12 Revised:2017-02-04 Online:2017-03-21 Published:2017-03-21

Abstract: A set of dolomitic reservoir developed in the Lower cretaceous A'ershan Formation of Bayindulan Sag,Erlian Basin. Based on the data of cores,cast thin sections,petrography,cathodoluminescence,SEM and Xray diffraction,the lithologies,reservoir spaces types,physical properties and diagenesis of the dolomitic reservoirs were studied. The result shows that the dolomitic reservoirs of A'ershan Formation can be divided into two types in lithology:dolomitic sandstone and dolomitic mudstone,and these two types of lithology can be divided into more types according to the occurrence of dolomite or ankerite. The dolomitic mudstone developed dissolved pores,fractures and intracrystalline pores. The porosity of dolomitic mudstone is 4.4%-36.4%,with an average of 16.01%,and the permeability is 0.01-26.30mD,with an average of 1.92 mD. The main reservoir spaces developed in dolomitic sandstone are dissolved pores. The porosity of dolomitic sandstone is 1.1%-33.7%,with an average of 16.07%,and the permeability is 0.01-5 163.00 mD,with an average of 79.72 mD. Replacement and dissolution are the main diagenesis types developed in dolomitic mudstone,and the diagenesis sequence is the formation of dolomite and ankerite→organic acid generation→dolomite dissolution. The main diagenesis types of dolomitic sandstone include dissolution,cementation and replacement, and the diagenesis sequence is:slight compaction→ quartz secondary overgrowth→cementation of dolomite and ankerite→organic acid generation→dissolution of dolomite,ankerite and feldspar.

CLC Number: 

  • TE122.2+3
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