structural evolution can be divided into three stages of chiasmic, depressed and abortion equilibrium.
构造演化可以分为裂陷阶段、沉陷阶段和萎缩平衡3个阶段。
The deposition of flysch onto the young floors of chiasmic basins is widely accepted as certain.
复理石的沉积作用发育在裂陷盆地年青底板上的看法被广泛接受.
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