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鄂尔多斯盆地庆城地区长7段致密砂岩成岩演化与孔隙结构特征
引用本文:王恩泽,吴忠宝,宋彦辰,石开波,刘航宇,刘波.鄂尔多斯盆地庆城地区长7段致密砂岩成岩演化与孔隙结构特征[J].北京大学学报(自然科学版),2022,58(2):249-260.
作者姓名:王恩泽  吴忠宝  宋彦辰  石开波  刘航宇  刘波
作者单位:1. 北京大学地球与空间科学学院, 北京 100871 2. 北京大学石油与天然气研究中心, 北京 100871 3. 中国石油勘探开发研究院, 北京 100083
基金项目:国家科技重大专项(2017ZX05013-006);
摘    要:利用薄片观察、扫描电子显微镜(SEM)观察、X射线衍射(XRD)分析和高压压汞实验等手段,系统地研究鄂尔多斯盆地庆城地区三叠系延长组七段(长7段)致密砂岩的岩性、物性、孔隙结构以及成岩作用特征,揭示孔隙结构和成岩作用对储层物性的控制作用,进而提出针对研究区长7段致密砂岩油储层的分级评价标准.长7段致密砂岩以长石岩屑砂岩...

关 键 词:致密砂岩  孔隙结构  分形特征  成岩演化  鄂尔多斯盆地
收稿时间:2021-03-12

Pore Structure and Diagenetic Evolution Features of Member-7 of Yanchang Formation in Qingcheng Area,Ordos Basin,NW China
WANG Enze,WU Zhongbao,SONG Yanchen,SHI Kaibo,LIU Hangyu,LIU Bo.Pore Structure and Diagenetic Evolution Features of Member-7 of Yanchang Formation in Qingcheng Area,Ordos Basin,NW China[J].Acta Scientiarum Naturalium Universitatis Pekinensis,2022,58(2):249-260.
Authors:WANG Enze  WU Zhongbao  SONG Yanchen  SHI Kaibo  LIU Hangyu  LIU Bo
Affiliation:1. School of Earth and Space Sciences, Peking University, Beijing 100871 2. Institute of Oil and Gas, Peking University, Beijing 100871 3. Research Institute of Petroleum Exploration and Development, China National Petroleum Corporation, Beijing 100083
Abstract:Thin section and scanning electron microscope (SEM) observations, X-ray Diffraction (XRD) measurements, and mercury intrusion capillary pressure were selected to systematically research the lithology, physical properties, pore structure, and diagenetic features of member-7 of Yanchang Formation (Chang-7 Fm) in Qingcheng Area, Ordos Basin, NW China. The influences of pore structure and diagenetic processes of physical properties were revealed, and the gradual evaluation standard was proposed. The results show that the Chang-7 Fm sandstones are dominated by feldspathic litharenites. The average porosity and permeability are 9.7% and 0.06 mD, respectively, which can be classified as a set of tight sandstone reservoir. The reservoirs stay in mesodiagenesis B stage, and the physical properties are primarily controlled by mechanical compaction and dissolution. The coarser particle size and higher content of quartz and feldspar improve the anti-compaction ability of relatively high-quality reservoirs. Meanwhile, quartz and feldspar also provide material basis for dissolution, and are important control factors for the development of relatively high-quality reservoirs. The pore type and structure also have influences to the physical properties. The primary pore has excellent connectivity. The development of secondary pores is conducive to porosity increasement, but has little effect to permeability. Based on the fractal theory, the heterogeneity of reservoir’s pore network is quantified, and the results show that the heterogeneity is negative correlate with the porosity and permeability, which means that the complex pore network is not conducive for the development of high-quality reservoirs. According to the pore structure and physical properties, three categories can be identified of the Chang-7 Fm tight sandstones. Class I and II reservoirs have large particle size, and the pore system is dominated by primary pores with less heterogeneity, therefore, they are favorable exploration targets. Type III reservoir has small particle size, and mainly develops intercrystalline pores of clay minerals, possess strong heterogeneity of pore structure and poor physical properties, which is not the target of tight oil and gas exploration.
Keywords:tight sandstone  pore structure  fractal characteristics  digenesis evolution  Ordos Basin  
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