在格伦维尔造山运动以后,加丹加造山运动之前(在1000—650百万年之间)形成的各种岩系都划归末原生代(Epiprotozoic)。在这个时期沉积杂岩内出现的冰川沉积物是该代沉积物的最重要特征。区域评述和主要岩系欧洲在欧洲,这个代的地层,大多数是地台和冒地槽型岩相。地台型岩相分布在俄罗斯地台和波罗的地盾的 After the Glenelg orogeny, various rock formations formed prior to the Katanga orogeny (between 1000-650 million years) were assigned to Epiprotozoic. The glacial deposits in sedimentary complexes during this period are the most important features of this generation of sediments. Regional Commentary and Main Rock Series Europe In Europe, most of the strata of this generation are platform stations and overrun trough facies. The platform type lithofacies are distributed on the Russian platform and the Baltic Shield