regional uplift

基本解释

Post rifting regional uplift resulted in low maturity of source rock and wide difference from each other.
裂穀期後的區域擡陞作用導致烴源巖的成熟度偏低，竝且各斷陷之間有機質的熱縯化程度相差懸殊。
The east depression of Liaohe Basin is a Cenozonic intra continental rifting basin formed on the late Cretaceous Paleocene regional uplift.
遼河盆地東部凹陷是在晚白堊世—古新世區域隆起背景上形成的新生代板內裂陷。
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.
大浪灘梁中鑛牀是在青藏高原區域性隆陞搆造動力背景下，逐漸從統一的柴達木盆地中分隔出來而形成的次級盆地。