盆地经历印支运动、燕山运动、喜山运动的改造。
This basin was reformed in Yinzhi movement, Yanshan movement and Ximalaya movement.
包体均一温度经压力校正后，可明显看出各储层油气的运移都发生在印支运动后的侏罗纪；
The pressure-corrected inclusion homogenization temperatures evidently show that the oil-gas migration in various reservoirs took place in the Jurassic after the Indosinian movement.
根据新测构造地质剖面资料，指出印支运动导致地台盖层和右江盆地构造层全面褶皱的主张是一大误解。
It is confirmed that the theory of the overall folds of the platform cover and the Youjiang basinal synthem of South China caused by the Indosinian movement is a great misunderstanding.
三叠纪末的印支运动结束了柴达木地块及其周缘地区的海相沉积史，使柴达木地区进入陆内盆地发育新时期。
At the end of Triassic period, the Marine sedimentation on Qaidam Massif (including its surroundings) has ended, and interior basin started to develop in Qaidam area.
川东石炭系中的天然气属于油型气，初为原油，曾经聚集于印支运动中形成的梁平—长寿古隆起带里，形成油藏。
The Carboniferous natural gas in eastern Sichuan is of cracked gas which had been accumulated, originally as oil, in Liangping-Changshou palaeohigh belt that was formed by Indosinian movement.
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.
印支、燕山、喜山运动使断裂带附近的油气藏破坏形成古油藏，但构造相对稳定地区的油气藏仍然得以保存。
After the Indosinian, Yanshan, and Himalayan movements, the previous pools near the faults were damaged, but that in the relatively stable areas were preserved.
班公湖-怒江带以北，表现为强烈的造山运动，形成规模巨大的印支造山带。
The movement performs in the form of strong orogeny north of Bangonghu-Nujiang suture, which leads to large-scale Indosinian orogenic belt.
班公湖-怒江带以北，表现为强烈的造山运动，形成规模巨大的印支造山带。
The movement performs in the form of strong orogeny north of Bangonghu-Nujiang suture, which leads to large-scale Indosinian orogenic belt.
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