central uplift belt

基本解释

In the central uplift belt, Upper Triassic-Middle Jurassic Fuzhou Formation provides major source rocks.
中央隆起带以上三叠统—中侏罗统福州组为主要烃源岩；
The central uplift belt underwent a series of structural evolution:fault block tilting, gravity slumping, inverse drag, rock salt uplifting and so on.
该带在形成过程中经历了块断抬斜、重力滑动、反拖牵引、盐岩拱升等多种形式的构造变动。
White Tiger oilfield, located on a faulted basement block along the Lower Cenozoic central uplift belt in Cuu Long basin, Vietnam, is mainly composed of granite and granodiorite.
白虎油田位于越南东南兰龙盆地早新生界中央隆起带基岩断块，以花岗岩和花岗闪长岩为主。