regional uplift

基本解釋

Post rifting regional uplift resulted in low maturity of source rock and wide difference from each other.
裂谷期后的區(qū)域抬升作用導(dǎo)致烴源巖的成熟度偏低，并且各斷陷之間有機質(zhì)的熱演化程度相差懸殊。
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(qū)域隆起背景上形成的新生代板內(nèi)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.
大浪灘梁中礦床是在青藏高原區(qū)域性隆升構(gòu)造動力背景下，逐漸從統(tǒng)一的柴達(dá)木盆地中分隔出來而形成的次級盆地。