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华庆地区长6 油层组黏土矿物类型及其对储层物性的影响
引用本文:周桦,黄思静,兰叶芳. 华庆地区长6 油层组黏土矿物类型及其对储层物性的影响[J]. 岩性油气藏, 2012, 24(3): 66-73. DOI: 10.3969/j.issn.1673-8926.2012.03.013
作者姓名:周桦  黄思静  兰叶芳
作者单位:1. 成都理工大学沉积地质研究院,四川成都610059; 2.成都理工大学油气藏地质及开发工程国家重点实验室,四川成都610059
基金项目:国家科技重大专项“鄂尔多斯盆地中生界延长组储层特征研究”(编号:2008ZX05001-004-003)资助
摘    要:在薄片、X 射线衍射和扫描电镜分析基础上,研究了鄂尔多斯盆地华庆地区长6 油层组砂岩中黏土 矿物的主要类型、赋存方式及其对储层物性的影响。结果表明:长6 油层组砂岩中的黏土矿物主要为绿 泥石、伊利石和混层伊利石/蒙皂石,黏土矿物总量平均为4.55%;自生绿泥石主要以孔隙衬里方式产出, 对深埋藏砂岩的储集空间具有显著的保护作用;伊利石和混层伊利石/蒙皂石主要以孔隙桥接或孔隙充填 方式产出,其大量存在会堵塞孔隙喉道、减小孔喉半径,从而对储层物性产生负面影响;高岭石在华庆地 区长6 油层组砂岩中不发育,是由于高含量杂基导致长6 油层组砂岩在酸性流体出现之前已基本完成压 实作用,且长7 烃源岩有机质演化过程中产生的酸性流体对其影响十分有限,使其缺乏足够的粒间孔隙 和活跃的酸性流体沉淀高岭石。

关 键 词:低渗透  非达西流  非达西渗流湍流系数  雷诺数  层流  湍流  

Types of clay minerals and its effects on reservoir properties of Chang 6 oil reservoir set in Huaqing area,Ordos Basin
ZHOU Hua,HUANG Sijing,LAN Yefang. Types of clay minerals and its effects on reservoir properties of Chang 6 oil reservoir set in Huaqing area,Ordos Basin[J]. Northwest Oil & Gas Exploration, 2012, 24(3): 66-73. DOI: 10.3969/j.issn.1673-8926.2012.03.013
Authors:ZHOU Hua  HUANG Sijing  LAN Yefang
Affiliation:1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China; 2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China
Abstract:Based on thin section analysis,X-ray diffraction and scanning electronic microscope analyses,this paper studied the types,occurrence of clay minerals and its influence on reservoir properties of Chang 6 oil reservoir set in Huaqing area.The result shows that the clay minerals in Chang 6 oil reservoir set mainly consist of chlorite,illite and illite/smectite mixed layer,and the average content of clay minerals is approximately 4.55%.Authigenic chlorite commonly occurs as pore-lining cement,which is beneficial to protect porosity of deeply buried sandstones.The occurrence of illite and illite/smectite mixed layer is pore bridging or pore filling,which will block up pore spaces and reduce throat radius,and have negative effect on sandstone reservoir.Authigenic kaolinite in Chang 6 oil reservoir set in Huaqing area is not developed.High matrix content makes the reservoir experience intense compaction earlier than acidic fluid,and the influence of acidic fluid from Chang 7 hydrocarbon rocks is limited for Chang 6 oil reservoir set,both of them result in the lack of intergranular volume and active acidic fluid for kaolinite.
Keywords:clay minerals  authigenic chlorite  X-ray diffraction  physical properties  Chang 6 oil reservoir set  Ordos Basin
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