Tectono -sedimentary evolution of the basin may be divided into three stages: continental margin rift, back-arc rift, and depression basin.
其沉积—构造演化可划分为三个阶段：大陆边缘裂谷、弧后裂谷和拗陷盆地。
Tectono - sedimentary evolution of the basin may be divided into three stages: continental margin rift, back-arc rift, and depression basin.
其沉积—构造演化可划分为三个阶段：大陆边缘裂谷、后裂谷和拗陷盆地。
Therefore, the Kuruktag ur-ocean rift and Manjaer original continental margin were proposed.
因此提出了库鲁克塔原洋裂谷和满加尔初始被动大陆边缘的新见解。
It caused the Youjiang basin evolved from continental rift basin to passive continental margin rift basin.
导致右江盆地由陆内裂陷盆地向被动陆缘裂谷盆地演化。
It caused the Youjiang basin evolved from continental rift basin to passive continental margin rift basin.
导致右江盆地由陆内裂陷盆地向被动陆缘裂谷盆地演化。
应用推荐