根据区域构造演化史提出岩溶演化模式，指出多期的构造旋回，复杂的断块掀斜作用和长期的化学活动性流体的溶蚀是研究区古岩溶发育的主要因素。
The main factors leading to the development of paleokarst in the region were found to be multi-phase tectonic cycle , complicated fault-block tilting and long-term dissolution by chemically active fluids .
化学活动性流体