Intermontane basins in relatively stable regions subjected to regional uplift.
较稳定区域内的山间盆地，曾有过区域隆起。
Post rifting regional uplift resulted in low maturity of source rock and wide difference from each other.
裂谷期后的区域抬升作用导致烃源岩的成熟度偏低，并且各断陷之间有机质的热演化程度相差悬殊。
The east depression of Liaohe Basin is a Cenozonic intra continental rifting basin formed on the late Cretaceous Paleocene regional uplift.
辽河盆地东部凹陷是在晚白垩世—古新世区域隆起背景上形成的新生代板内裂陷。
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