摘要
本文以水、岩相互作用的观点,应用古水文地质分析原理,从岩溶演化角度,探讨四川南部二叠系阳新灰岩中的有关岩溶现象。指出阳新灰岩储层受岩溶控制,是长期岩溶作用叠加的产物。
In view of interaction of water and rocks, the development of the karst of yangxin limestone in South Sichuan is discussed with the analysis method used. It is put forward that the reservior of Yangxin series is controlled by the karst, which results from the accumulation of the karst formation in a long period.
关键词
二叠纪
灰岩
岩溶
发育
演化
limestone
karst
reservoirs stratum/Yiangxin limestone
