苏加塔湖谷属于东非裂谷系统,那里的构造板块正在相互分离开。
The lake valley lies within the East African Rift System, where tectonic plates are moving away from each other.
东非裂谷系开始在北部叙利亚和延伸穿过东非到莫桑比克。
The East African Rift Valley system begins in northern Syria and extends across East Africa into Mozambique.
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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