准噶尔盆地西北缘克百地区三叠系储层溶蚀作用特征及孔隙演化
- 收稿日期:
1900-01-01
- 修回日期:
1900-01-01
- 刊出日期:
2010-06-10
摘要: 基于岩石薄片、铸体薄片、扫描电镜等镜下特征分析,对准噶尔盆地西北缘克百地区三叠系溶蚀作用特征进行了系统的分析。三叠系溶蚀作用发育普遍、现象丰富、对储层改造作用明显,是研究区最为重要的成岩作用类型。“成分成熟度低、结构成熟度中等偏下”的岩石学特征是成岩作用的沉积基础。长石的溶蚀在该区最为常见,胶结作用弱、局部见方解石和方沸石溶蚀,碱性条件下石英弱溶蚀。溶蚀作用对储层的改造决定了克百断裂上、下盘三叠系储层的孔隙空间类型和孔隙的垂向演化。岩石类型、泥质含量和沉积微相等因素控制储层中溶蚀作用的发育程度及分布。
Dissolution Characteristics and Pore Evolution of Triassic Reservoir in KeBai Area, Northwestern Margin of Junggar Basin
- State Key Laboratory of Petroleum Resource and Prospecting, Beijing 102249
- Received Date:
1900-01-01
- Rev Recd Date:
1900-01-01
- Publish Date:
2010-06-10
Abstract: Based on a large number of thinsections, casting thinsections and scanning electron photomicrographs observation , the characteristics of Triassic dissolution in KeBai area, northwestern margin of Junggar Basin are systematically studied. Triassic dissolution is generally developed in KeBai area, with abundant typical phenomena, and reservoir is obviously reformed , so dissolution is the most important type of diagenesis in the study area. The lithology characteristics of "low compositional maturity, lowermiddle textural maturity " provide a sedimentary basis for diagenesis. The dissolution of feldspar is the most common in the area, and cementation is weak, with little calcite and analcime dissolution, quartz is slightly dissolved under alkaline condition. The type of pore space and the vertical evolution of porosity on different walls of the fault belt are determined by dissolution. The intensity and distribution of dissolution was affected by the rock type, matrix content, microfacies and other factors.
朱世发. 准噶尔盆地西北缘克百地区三叠系储层溶蚀作用特征及孔隙演化[J]. 沉积学报, 2010, 28(3): 547-555.
引用本文: |
朱世发. 准噶尔盆地西北缘克百地区三叠系储层溶蚀作用特征及孔隙演化[J]. 沉积学报, 2010, 28(3): 547-555.
|
ZHU Shifa. Dissolution Characteristics and Pore Evolution of Triassic Reservoir in KeBai Area, Northwestern Margin of Junggar Basin[J]. Acta Sedimentologica Sinica, 2010, 28(3): 547-555.
Citation: |
ZHU Shifa. Dissolution Characteristics and Pore Evolution of Triassic Reservoir in KeBai Area, Northwestern Margin of Junggar Basin[J]. Acta Sedimentologica Sinica, 2010, 28(3): 547-555.
|