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从构造与非构造作用角度出发,突出研究断层对裂缝的控制作用、断裂与岩溶的关系和裂缝与岩溶之间的关系,揭示碳酸盐岩裂缝与岩溶的发育规律。研究表明:构造裂缝为岩溶发育提供岩溶作用进行的有利通道,非构造裂缝则可以加速溶蚀作用的进行,促进岩溶的发育;裂缝与岩溶之间的关系始终是相辅相成、相互促进的关系。
From the perspectives of tectonics and non-tectonics, the study focused on the study of the role of faults in controlling fractures, the relationship between faults and karst, and the relationship between fractures and karst, revealing the development of carbonate fractures and karst. The results show that tectonic fractures provide a favorable channel for karstification development, while non-tectonic fractures accelerate the dissolution and promote the development of karst. The relationship between fractures and karstification is always complementary and mutually reinforcing.