Molasse

基本解释

The molasse sediments consist of two categories: marine and continental.
磨拉石沉积可分为海相含煤磨拉石和陆相红色磨拉石两种类型。
Huge thick Cathysian formations (Molasse strata) with certain terrestrial flysch rhythm were deposited and lots of eruptive rock formations were intercalated in these basins.
在这些盆地中沉积了巨厚层的、具有一定陆相复理式韵律的华夏式建造,并夹杂着大量的火山喷发岩建造。
Evaporite formation altogether with its underlying molasse formation forms a complete metallogenic system for strata-bound deposits.
蒸发岩建造;包括其下的磨拉石建造构成了一个完整的层控铜、铅、锌矿床所必需的成矿系统.
The Fe Mn mass dissociated by weathering in the red molasse formation can partly adjust the pH of sedimentary environments.
而红色磨拉石建造中风化离解的Fe，Mn物质对沉淀环境pH值起着一定的调节作用。
In the Dajiuba region, the Late Palaeozoic stable covers, ophiolite complex and the Early Permian foreland molasse basin sediment are exposed.
晚三叠世陆相火山岩出露于祁漫塔格山南缘。