文章详细信息 关键词： 晚三叠世;;磨拉石;;兴蒙-吉黑造山带;;中国东北 [gap=1219]Keywords: Late Triassic;molasse;Xing'an-Mongolian-Ji-Hei orogenic belt;Northeast China
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molasse formation 磨拉石建造
molasse face 磨砾岩相
molasse facies 磨拉石相
molasse clastic basin 磨拉石碎屑盆地
molasse-type sediment 磨拉石型沉积
molasse e 磨砾层
molasse basin 磨砾层
afterdeep molasse 后渊磨拉石
exhausted molasse 废糖蜜 ; 桔蜜
N a soft sediment produced by the erosion of mountain ranges after the final phase of mountain building 磨砾层
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。
Cenozoic molasse at the south edge of Qinghai-Tibetan Plateau was mostly deposited in the zones of Lesser-Himalaya and Sub-Himalaya, others in Alluvial Plain zone.
青藏高原南缘前陆盆地中的磨拉石主要沉积在小喜马拉雅带和次喜马拉雅带中，次之出现在冲积平原带。
On the southwestern margin of the basin there occur middle Yanshanian Late Triassic and Early Cretaceous coarse clastic molasse-like deposits and angular unconformity.
在盆地西南缘发育燕山中期的晚侏罗世和早白垩世的粗碎屑类磨拉石建造及其地层间的角度不整合。
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