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芬兰西南部古元古代库提马加威金碲化物矿床热液流体的演化１区域地质芬诺斯坎德地盾的斯韦考芬构造域大约是在１．９Ｇａ时由地壳快速增生形成的．坦佩雷片岩带位于地盾中部，其北部是大面积的花岗岩类（１．８９±０．０１Ｇａ），南部是瓦马拉混合岩带．ＳｍＮｄ同位素...
Evolution of the hydrothermal fluid in the ancient Paleoproterozoic gold telluride deposit in southwestern Finland 1 The regional geology of the Venuskander shield is formed by rapid crustal growth at 1.9 Ga . The Tampere schist belt is located in the middle of the shield. Its northern part is a large-scale granitoids (1.89 ± 0.01Ga) and the southern part is the Vamara mixed belt. SmNd isotope ...