molasse

The Meishan group of Carboniferous system has the nature of molasse formation .

石炭系梅山群具磨拉石建造特征。

Late early Permian Epoch molasse formation ;

早二叠世晚期的磨拉石建造；

Its age is late Early Triassic . Late early Permian Epoch molasse formation ;

其时代为早三叠世晚期。

The structure forms of Maoshan fault zone and the discovering of the tectonic hybrid rocks and molasse

茅山断裂带结构和构造混杂岩带及磨砾岩之发现

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。

Molasse is a sedimentary assemblage which is characteristic of clastic sediments and rapid accumulation on the front of mountain mass .

磨拉石可定义为以碎屑沉积为特征的、在隆起的山体前缘快速堆积为沉积组合。

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。

Molasse and global tectonics

磨拉石与全球构造

In Early Carnian of the Late Triassic , molasse sediments developed , and shelf , slope and basin deposits only occurred in local areas .

晚三叠世卡尼早期因东侧金沙江洋的消亡，发育磨拉石沉积，仅在局部地区表现为陆棚→斜坡→盆地沉积；

The discovery of molasse facies deposits of the Caledonides in southwestern Jiangxi " I should have brought a stone . "

赣西南加里东造山带磨拉石相沉积的发现

The Lixian-Minxian foreland basin undertook abyssal-bathyal flysch deposition at its earlier evolution stage and continental molasse stage at its later evolution stage .

礼岷前陆盆地经历了早期深海&半深海的复理石沉积阶段和晚期陆相磨拉石沉积阶段。

J 3 & K 1 , the stage of forming oxidized broad and shallow lake and red Molasse formation is that of beneficial reservoirs growing in central and west China ;

J3-K1时期为氧化宽浅湖与红色磨拉石建造期，是中西部地区有利储集层的发育时期；

The third one , formed at early stage of later-Proterozoic ( 1000-800Ma ), was belong to molasse formation accumulated in foredeep or intermountain basin ;

晚元古界早期构造层，为山前凹地或山间盆地磨拉石堆积，形成于1000-800Ma；

The Chuxiong Basin is a Mesozoic foreland basin in central Yunnan . The sediments in the basin may fall into two subtypes : foreland flysch and foreland molasse .

楚雄盆地位于云南省的中部，为一中生代的前陆盆地，其沉积可划分为前陆复理石和前陆磨拉石两个阶段。

2000-3000 m of molasse started in the late Miocene and with a coarsening-up tendency show a rapid and accelerated uplifting from the late Miocene to early Pleistocene .

从中新世后期开始的厚达2000～3000m的磨拉石沉积，其粒度向上加大，显示从中新世后期到早更新世隆升速率高而且是加速的。

Detailed sedimentary research indicates that Late Jurassic Mohe basin contains the alluvial fan , fan-delta and lacustrine facies , belonging to continental molasse deposits of the foreland basin .

详细的沉积学研究表明：晚侏罗世漠河盆地主要发育冲积扇、扇三角洲和湖泊相沉积，属于前陆盆地的陆相磨拉石部分。

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。

The Late Permian-Middle Triassic succession of the basin is composed of thick , coarse molasse deposits and fine clastics , organized into coarsening-upward and fining-upward stratigraphic sequences .

十万大山盆地晚二叠世&中三叠世沉积由巨厚的磨拉石建造组成，并构成多个向上变粗和向上变细的构造-地层层序。

The three types of molasse are genetically related to the models of Welson mountain building cycles , on the account of : 1.different types of molasse formed in different stages of Welson cycles ;

上述三类磨拉石与威尔逊造山旋回模式之间有着成因联系，表现为：1。威尔逊旋回的不同阶段形成不同类型的磨拉石；

2 ) flourishing stage ( T2-T3 ), during which the marine foreland develops to continental foreland , forming marine molasse and continental molasse ; ( 3 ) molasse deposits ;

2）兴盛阶段（T2&T3），由海相前陆盆地向陆相前陆盆地转化，发育海相和陆相磨拉石沉积；

The basin was migrated northward in Late Jurassic , and in the piedmont basins with EW and NE directions in the southern and eastern parts of Inner Mongolian Axis , the substance from adjacent mountainous areas was deposited , forming the molasse formation ;

晚侏罗世的盆地往北推移，在内蒙地轴南部及东部的E&W向及NE向的山间盆地中，接受了周边山地的物源而形成磨拉石建造；