第四纪盆地稳定沉降阶段为生物气聚集成藏时期。
The steady (subsidence) stage of the Quaternary was the period of biogas accumulation.
上新世-第四纪区域沉降阶段，东西向断层再次活动。
Regional subsidence stage from Pliocene to Quaternary, the EW trending reactivated.
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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