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。
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。
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。
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。
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。
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