n.復(fù)理層(厚砂頁巖夾層)

The deposition of flysch onto the young floors of chiasmic basins is widely accepted as certain. 復(fù)理石的沉積作用發(fā)育在裂陷盆地年青底板上的看法被廣泛接受。

The clastic rocks widespread in the Triassic Xikang Group in western Sichuan consist dominantly of turbiditic flysch formations. 摘要三疊系西康群碎屑巖主體為一套濁積巖復(fù)理石建造。

In the south area, there are mainly flysch and deep sea facies fossil, such as Graptolites in fossil feature. 南區(qū)巖性為復(fù)理石建造，生物以深海相筆石為主。

Huge thick Cathysian formations (Molasse strata) with certain terrestrial flysch rhythm were deposited and lots of eruptive rock formations were intercalated in these basins. 在這些盆地中沉積了巨厚層的、具有一定陸相復(fù)理式韻律的華夏式建造,并夾雜著大量的火山噴發(fā)巖建造。

The Liufengguang flysch here refers to the early Triassic flysch formation of the Liufengguang group in the East Qinling miogeosyncline. 正>留鳳關(guān)復(fù)理石,系指東秦嶺冒地槽早三迭世留鳳關(guān)群的復(fù)理石建造。它位于寶成鐵路的鳳縣至聶家灣一帶(圖1),向西延至西秦嶺。