晚中新世以后，盆地进入浅海半深海沉积环境的裂后热沉降期。
After Late Miocene, the basin got into a post_rift thermal subsidence stage in a shallow to semi_deep sea environment.
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.
而南苏丹裂谷进入后裂谷热沉降阶段是与新生代东非裂谷带和红海的发育分不开的。
The authors also conclude that the South Sudan Rift entered the post-rift thermal sag phase because of the development and evolution of the East African Rift and Red Sea in the Cenozoic.
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