Pore types, origins and control on reservoir heterogeneity of carbonate rocks in Middle Cretaceous Mishrif Formation of the West Qurna oilfield, Iraq

被引:34
|
作者
Liu, Hangyu [1 ]
Tian, Zhongyuan [2 ]
Liu, Bo [3 ]
Guo, Rui [2 ]
Yang, Di [4 ]
Deng, Ya [2 ]
Yu, Yichang [2 ]
Shi, Kaibo [1 ]
机构
[1] Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China
[2] PetroChina, Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China
[3] Peking Univ, Oil & Gas Res Ctr, Beijing 100871, Peoples R China
[4] China Univ Petr, Coll Geosci, Beijing 102249, Peoples R China
基金
中国国家自然科学基金;
关键词
Pore types; Pore origins; Reservoir heterogeneity; Carbonates; Mishrif Formation; West Qurna oilfield; SOUTHERN MESOPOTAMIAN BASIN; RUDIST-BEARING CARBONATES; TIGHT SANDSTONES; ARABIAN GULF; CLASSIFICATION; SEQUENCE; FEATURES; GENESIS; SPACE;
D O I
10.1016/j.petrol.2018.08.034
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
Carbonates in Upper Cretaceous Mishrif Formation of the West Qurna oilfield in Iraq are characterized by complicated rocks and pores types, and strong heterogeneity. Based on the cores and cast thin sections of three wells, pore types were identified, and pore origins were analyzed from the perspective of sedimentary and diagenesis features. Porosity and permeability measurement, and high pressure mercury injection capillary pressure tests were conducted to determine the relationships between pores and reservoir heterogeneity. Six types of pores are identified, and they are intragranular pores, moldic pores, residual moldic pores, intergranular pores, micropores and intercrystal pores. The pore origins were controlled by the sedimentary environments and diagenesis. Pore types were controlled by lime mud contents, bioclastic textures, types and abundance that were controlled by sedimentary environments. Pore occurrence was determined by various diagenesis, while pore occurrence was mainly attributed to dissolution, which was influenced by the mineral composition of bioclastics. In addition, pores were altered by micritization, cementation and compaction. Results from the comparison of reservoir parameters show that the reservoir physical properties and pore structure of the each dominant pore type are similar. The study proves that reservoir characteristics are controlled by dominant pore types and reveals that pore type is a crucial cause for strong reservoir heterogeneity of carbonates.
引用
收藏
页码:1338 / 1349
页数:12
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