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溶蚀作用
[地理][地质] dissolution
- 普遍认为酸性流体的溶蚀作用是碳酸盐岩储层形成的重要制约因素。
It is thought generally that dissolution of acidic fluids is an important controlling factor for forming carbonate reservoir. - 溶蚀作用受岩性、古油藏抬升受破坏程度以及与断层的关系控制。
Dissolution was controlled by lithology, the destructiveness of the uplifted fossil reservoirs and their relationship with faults. - 成岩早期胶结作用形成剩余原生粒间孔，晚期的溶蚀作用形成次生孔隙。
Residual original intergranular pore developed during early diagenesis of sandstone, secondary pore was created by dissolution in late diagenesis .
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