岩性油气藏 ›› 2021, Vol. 33 ›› Issue (2): 116126.doi: 10.12108/yxyqc.20210212
张治恒1, 田继军1, 韩长城1, 张文文1, 邓守伟2, 孙国祥2
ZHANG Zhiheng1, TIAN Jijun1, HAN Changcheng1, ZHANG Wenwen1, DENG Shouwei2, SUN Guoxiang2
摘要: 为研究吉木萨尔凹陷芦草沟组页岩油储层特征及主控因素,开展岩心观察、铸体薄片鉴定、扫描电镜分析及全岩分析等工作,研究其岩石学特征、物性特征和成岩作用等。结果表明:芦草沟组岩石类型主要为碎屑岩、碳酸盐岩和混合细粒岩等,成分成熟度和结构成熟度均较低,分选性中等,原生粒间孔和次生溶孔是主要储集空间,砂岩孔隙度平均为7.34%,渗透率平均为0.079 mD,属低渗致密储层;储层发育主要受沉积和成岩双重作用控制,其中沉积作用控制着储层岩石类型的发育和分布,成岩作用过程中压实作用和胶结作用是导致储层孔隙度下降的主要原因,溶蚀作用对储层物性条件起到一定的改善作用。芦草沟组储层共经历了3次致密化阶段,压实作用是早期致密的主要原因,持续压实作用和硅质胶结作用在中期致密化阶段起到主导作用,晚期压实作用和碳酸盐岩、黏土矿物胶结共同作用于储层,使储层进一步致密化。该成果可为开发吉木萨尔凹陷芦草沟组页岩油提供一定理论依据。
中图分类号:
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