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铀矿化体产于瑞士格劳宾登前莱茵河谷施兰斯村南坡脚提劳恩地区的碎屑岩中。该矿点是1962年发现的,已打了三个浅钻孔。本文报道对提劳恩铀矿点的一组标本所进行的岩石学、矿物学及 X 光研究结果。并对距其西南约1.5公里,产状相似的特伦矿点做了对比研究。特伦矿点产于塔韦茨山的变质岩中,其主要矿化年龄为303—329百万年,据认为矿化是在华力西变质作用期间的高温热液条件下,由于近矿围岩中金属的活化而形成的。
Uranium mineralized production in the Swiss Graubunden former Rhine Valley Schrans village on the southern slope of the slope to Laun region clastic rocks. The mine was discovered in 1962 and has hit three shallow holes. This paper reports on the petrology, mineralogy and X-ray results of a group of specimens from the Tirau uranium mine. And about 1.5 km from its southwest, similar to the occurrence of the Tron mine to do a comparative study. The Tron Mine is produced in the metamorphic rocks of the Taweici Mountain and its main mineralization age is 303-329 million years. It is believed that the mineralization is due to the high temperature hydrothermal conditions during the metamorphism of the Variscan, Surrounding rocks formed by the activation of the metal.