The sedimentary evolution and paleostructure in the western Qaidam Basin were discussed by combining dynamic and whole states.
利用动态联系与整体相结合的思路，分析了柴达木盆地西部地区沉积演化和古构造特征，确定了该地区主要成藏期。
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。
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