1、

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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2、

The deep-water in situ deposits and deep-water allogene deposits develop flysch rhythmic sequences.

深水原地沉积与异地沉积在剖面上组成了复杂的复理石韵律.

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3、

The marine flysch deposition of early foreland basin appeared in Indosinian; owing to early Indosinian movement the sand mudstones ( T 2) were folded into mountains, which made the late foreland basin be withered away;

印支期出现早期前陆盆地海相复理石沉积,由于早印支运动使T2砂泥岩揉褶成山,晚期前陆盆地夭折。

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