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.
第三阶段，中、晚中新世随着印度地块逐渐楔入欧亚板块内部，印支半岛的挤出运动进一步减弱。
The third phase, during the middle and the later Miocene, with the Indochina block intruding into Eurasia plate gradually, Indochina peninsula's extrusion slowed down further.
统一陆壳也是显生宙以来逐步形成的：主要经历了加里东和华里西-印支两大构造阶段。
The Qinghai crust was gradually collaged during the Paleozoic and mainly underwent Caledonian and Hercynian-Indosinian tectonic events.
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