芬兰挪威斯堪的纳维亚地盾,属波罗的地盾的最西部分,从北东芬兰和科拉太古代地核向西南挪威晚元古代省,依次过渡为年轻造山带。这后一个省通常称为瑞典挪威造山省(Kartz等,1968),但其在瑞典部分多使用Dalsandia这一名称(Magnusson,1960)。放射性测年表明,瑞典挪威期造山运动发生在1200—850m.y.,恰与加拿大地盾格林维尔造山运动的时代相当。 Finland Norway The Scandinavian Shield, which is the westernmost part of the Baltic Shield, is a transition to a young orogen in turn from North Eastern Finland and the Kola Archean to the late Proterozoic province of South West Norway. This latter province is commonly referred to as the Norwegian Norwegian orogen (Kartz et al., 1968) but uses the Dalsandia name more often in the Swedish part of the country (Magnusson, 1960). Radioactive dating shows that the Norwegian orogeny occurred in 1200-850m.y., Just as the Canadian Greenpeace orogeny era.