迈卢特盆地是苏丹东南部中—新生代的一个大型陆内裂谷盆地。
Melut Basin is a large-scale basin of the Cretaceous-Paleogene sediment in the southeastern Sudan.
导致右江盆地由陆内裂陷盆地向被动陆缘裂谷盆地演化。
It caused the Youjiang basin evolved from continental rift basin to passive continental margin rift basin.
盆地构造演化经历了前陆盆地和陆内盆地两个大阶段，后者又进一步分为陆内裂谷时期、再生前陆盆地时期和盆地消亡时期。
It has two tectonic evolutionary stages of foreland basin and intracontinental basin that is further divided into three periods of intracontinental rift, newborn foreland basin and dying out basin.
盆地构造演化经历了前陆盆地和陆内盆地两个大阶段，后者又进一步分为陆内裂谷时期、再生前陆盆地时期和盆地消亡时期。
It has two tectonic evolutionary stages of foreland basin and intracontinental basin that is further divided into three periods of intracontinental rift, newborn foreland basin and dying out basin.
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