复理

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1.

Thus, the syn-sedimentary compression structures can provide new evidences and constraints on the dynamic evolution of flysch basins .

这些构造为复理石盆地的动态演化研究提供了新的证据。

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.

Preliminary Approach to the Geotectonic Setting of Carboniferous Flysch Deposits in East Kunlun Mountains

东昆仑石炭系复理石沉积的大地构造背景初探

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4.

Tectonic setting and provenance of the Kudi flysch in west Kunlun mountains, Xingjiang province

新疆西昆仑库地复理石源区性质及构造背景分析

5.

Progressive flysch melt , mm devolatilization

复理石不断熔融，变质去挥发份

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6.

Internal-tide Deposits of Upper Ordovician Flysch in Linan Area of Zhejiang Province

浙江临安上奥陶统复理石中的内潮汐沉积

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7.

Features of Sandstone in the Yajiang Flysch Basin in West Sichuan in the Late Triassic

川西雅江晚三叠世复理石盆地砂岩特征

8.

New progress in the method of mapping of flysch areas in western Sichuan

川西复理石区填图方法的新进展

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