海西-印支期，华南地质构造发展进入新的阶段。
The geologic history of the South China developed into a new stage in the Hercynian - Indochina period.
在琼库恰克构造带的形成和发展过程中经历了海西运动期古构造形成阶段及喜马拉雅运动期现今构造定型阶段。
The formation and development of Qongkuqak structural zone underwent two stages, i. e. , Hercynian paleostructural forming stage and Himalayan present-structural forming stage.
以构造动力成矿系统理论为基础，通过构造成因及演化过程说明海西-燕山期是充水裂隙形成的重要阶段；
The structural information and evolution of the fissured-water pour-in on the basis of theory about Zhaoping structure mineralized dynamic system are analyzed.
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