regional uplift

基本解释

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。
The Dalangtan Liangzhong deposit is a secondary basin gradually divided from the united Qaidam Basin, under the background of Qinghai-Tibet Plateau's regional uplift tectonic motion.
大浪滩梁中矿床是在青藏高原区域性隆升构造动力背景下，逐渐从统一的柴达木盆地中分隔出来而形成的次级盆地。