填满裂缝的一般来说最普遍的就是水，因此促进了溶解。
Water is most often the substance that fills the voids and thus liquefaction is facilitated.
缝洞系统是在东吴期古溶洞系统基础上，经埋藏后充填和溶解，最后由喜山期构造裂缝改造而成。
The geological model of the reservoirs could be described as a combination of tubular caves system of Dongwu stage and Himalaya tectonic fracture network.
由模拟结果分析得出，岩盐水压致裂溶解过程裂缝的扩张以及裂缝宽度的变化受水压和溶解双重因素的影响。
The result indicates that the expansion and the width change of cracks are affected by hydraulic pressure and solution.
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