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安塞地区长8段储层成岩作用及孔隙定量演化

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通过铸体薄片鉴定、扫描电镜分析等方法,在储层基本特征、成岩作用与成岩序列分析的基础上,对安塞地区长 8 段储层的孔隙演化进行定量分析,建立储层孔隙演化模式.研究表明:压实作用对储层的破坏性最强,是储层致密的主要原因,减孔 67.56%;胶结作用减孔 23.65%,是储层在中成岩A期达到致密的关键;溶蚀作用则对储层物性具有一定的改善作用,在一定程度上延缓储层致密化的进程,增孔1.47%.孔隙演化在早成岩A期经历了快速压实—早期胶结阶段,在早成岩B期经历了压实减缓—早期溶蚀阶段,在中成岩A期经历了溶蚀—胶结致密阶段.该研究为安塞地区长 8 油层组下一步勘探开发提供依据.
Diagenesis and Pore Evolution of Chang 8 Reservoir in Ansai Area
Based on the analysis of reservoir basic characteristics,diagenetic processes,and diagenetic sequences through methods such as thin section identification and scanning electron microscope analysis,the pore evolution of the Chang 8 reservoir in the Ansai area was quantitatively analyzed and a reservoir pore evolution model was established.The research indicates that compaction is the most destructive to the reservoir,being the primary cause of its tightness,reducing porosity by 67.56%.Cementation reduces porosity by 23.65%and is the key factor in achieving tightness during the mid-diagenetic phase A.Dissolution,on the other hand,has a certain ameliorative effect on the reservoir properties,partially slowing down the process of reservoir tightness and increasing porosity by 1.47%.The pore evolution underwent a rapid compaction-early cementation stage during the early diagenetic phase A,followed by a compaction slowing-early dissolution stage in the early diagenetic phase B,and finally an erosion-cementation densification stage during the mid-diagenetic phase A.This study provides a basis for the next step of exploration and development of the Chang 8 reservoir in the Ansai area.

pore evolutiondiagenesisAnsai areaYanchang FormationOrdos Basin

龚金祥、廖明光、孙博、蒋汶卓、陈艺娴

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西南石油大学 地球科学与技术学院,四川 成都 610500

中国石油天然气股份有限公司长庆油田分公司第二采油厂,甘肃 庆阳 745100

孔隙演化 成岩作用 安塞地区 延长组 鄂尔多斯盆地

2024

河北地质大学学报
石家庄经济学院

河北地质大学学报

CHSSCD
影响因子:0.287
ISSN:1007-6875
年,卷(期):2024.47(4)