... 反向〔环流〕圈 reverse cell 反转期 reverse epoch 逆断层 reverse fault; reversed fault ...
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中国东北晚中生代经历了区域性的裂谷期、后裂谷热沉降期和反转期。
NE China experienced regional rifting, post-rifting thermal subsidence and thermal reverse in Late Mesozoic.
结果表明，断裂的主反转期是早第三纪早期，构造反转结束于早第三纪中晚期。
The results of discussion show that the main inversion period of the fault occurred in early Tertiary and the structure inversion ended in the middle and late periods of early Tertiary.
对塔里木盆地北部隆起轮台断裂带进行的实例分析表明，轮台负反转断裂主反转期为中新世苏维依期一吉迪克期，反转率为0．85～0．98。
Taking Luntai fault belt of northern Tarim uplift as an example, the main negative inversion phase of the fault may be Suwiyi-Jidike epoch of Miocene, and the inversion ratio is 0.85~0.98.
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