Oil & Gas Geology ›› 2025, Vol. 46 ›› Issue (3): 809-826.doi: 10.11743/ogg20250308
• Petroleum Geology • Previous Articles Next Articles
Qian TAN1,2(
), Haifeng YUAN1,2(
), Tao WANG2, Zili MA2, Bojun TANG2, Qiu PENG3, Wenjie LI1,2
Received:2024-12-30
Revised:2025-04-14
Online:2025-06-30
Published:2025-06-26
Contact:
Haifeng YUAN
E-mail:799285676@qq.com;yuanhaifeng08@cdut.cn
CLC Number:
Qian TAN, Haifeng YUAN, Tao WANG, Zili MA, Bojun TANG, Qiu PENG, Wenjie LI. Genesis and impact of dissolution in deep dolomite reservoirs: A case of the 2nd member of the Sinian Dengying Formation, Penglai area, central Sichuan Basin[J]. Oil & Gas Geology, 2025, 46(3): 809-826.
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Table 1
Characteristics and reservoir-controlling effects of multistage dissolution in the Deng 2 Member, Penglai area, central Sichuan Basin"
| 溶蚀作用类型 | 储层岩石学特征 | 分布规律 | 储层空间类型 | 典型胶结物类型 | 溶蚀机理 | 控储效应 |
|---|---|---|---|---|---|---|
| 同生期—准同生期溶蚀 | 向上变浅的沉积旋回的叠层石白云岩、凝块石白云岩和泡沫状绵层石白云岩 | 在台缘和台内丘滩广泛分布,呈多套叠置、韵律性分布 | 组构选择性溶蚀孔和网格状溶蚀孔洞 | FFD+RFD+晶粒白云石 | 周期性海平面变化驱动的短暂暴露;溶蚀流体以大气淡水和混合水为主 | 形成孔隙-孔洞型储层,是储层形成的基础 |
| 风化壳岩溶 | 岩溶角砾白云岩、凝块石白云岩、泡沫状绵层石白云岩和砂屑白云岩 | 主要分布岩溶斜坡之下的丘滩沉积中 | 溶洞和蜂窝状溶蚀孔洞 | FSD+RSD+晶粒白云石 | 桐湾运动引起的长时间暴露;溶蚀流体为大气淡水 | 形成孔洞型储层,是储层形成的关键 |
| 热液溶蚀 | 构造角砾白云岩、凝块石白云岩、泡沫状绵层石白云岩和砂屑白云岩 | 主要分布在东西向走滑断裂附近的丘滩沉积中 | 高角度缝洞 | 粗晶白云石+石英+萤石、方铅矿和闪锌矿 | 与峨眉山火山活动引起的热事件有关;溶蚀流体为富CO2热液 | 形成缝洞型储层,是储集空间重新分配的重要控制因素 |
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