岩性油气藏 ›› 2017, Vol. 29 ›› Issue (3): 2733.doi: 10.3969/j.issn.1673-8926.2017.03.004
闫林1, 冉启全1, 高阳2, 陈福利1, 王少军1, 李崇飞1
YAN Lin1, RAN Qiquan1, GAO Yang2, CHEN Fuli1, WANG Shaojun1, LI Chongfei1
摘要: 针对吉木萨尔凹陷芦草沟组致密油储层溶蚀孔隙较发育,但控制因素及成因机理认识程度低的问题,利用岩心、铸体薄片和扫描电镜观察以及物性测试等方法,结合矿物成分、油气成藏演化和成岩演化等分析,对研究区孔隙类型及特征、溶蚀孔隙成因机理及分布规律进行了研究。结果表明:吉木萨尔凹陷芦草沟组致密油陆源碎屑岩、内源沉积岩及火山碎屑岩3种岩石类型储层中均发育有溶蚀孔隙,其形成受内部和外部因素共同制约,有机酸溶蚀长石类及碳酸盐岩类等易溶矿物组分是其形成的主要方式;芦草沟组二段中部的岩屑长石粉细砂岩储层溶蚀孔隙发育程度高、物性好、厚度相对较大、平面分布较为稳定,是下一步致密油勘探开发的重点层位。
中图分类号:
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