central uplift belt

基本解释

In the central uplift belt, Upper Triassic-Middle Jurassic Fuzhou Formation provides major source rocks.
中央隆起帶以上三曡統—中侏羅統福州組爲主要烴源巖；
The central uplift belt underwent a series of structural evolution:fault block tilting, gravity slumping, inverse drag, rock salt uplifting and so on.
該帶在形成過程中經歷了塊斷擡斜、重力滑動、反拖牽引、鹽巖拱陞等多種形式的搆造變動。
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.
白虎油田位於越南東南蘭龍盆地早新生界中央隆起帶基巖斷塊，以花崗巖和花崗閃長巖爲主。