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欧洲前寒武系发育最好的地区是东欧地台及其邻近的褶皱带。如波罗的地盾(在北欧或称芬诺斯堪的纳维亚地盾)、乌克兰地盾(在乌克兰或称亚速-波多尔斯克)、俄罗斯台坪。地台镶边的褶皱带,如乌拉尔的海西褶皱带,北欧的加里东褶皱带中前寒武系分布广泛。在西欧北部的大不列颠及爱尔兰、中部法国地块、西班牙的西部和南部、中欧的波希米亚地块、巴尔干半岛的南部等地都有前寒武纪沉积分布,特别是苏联的科拉半岛、卡累利阿地区、斯匹茨卑尔根群岛及乌拉尔等地都有前寒武纪沉积比较完善的层型剖面。
The best developed area of the Precambrian in Europe is the Eastern Europe platform and its adjacent fold belt. Such as the Baltic Shield (in the Nordic or Finnish Scandinavian Shield), the Ukrainian shield (in Ukraine or the Azov-Podolsk), and the Taiping in Russia. Fold belts on the platform, such as the Hercynian fold belt in the Ural, and the Precambrian distribution in the Caledonian fold belt in northern Europe. Pre-Cambrian sedimentary facies have been distributed in Great Britain and Ireland in northern Western Europe, the French territories in central France, western and southern Spain, the Central European Bohemian massif and the southern Balkan Peninsula, especially the Kola Peninsula in the Soviet Union , The Karelia region, the Spitsbergen islands and the Ural and other places have pre-Cambrian sedimentary relatively well stratified profile.