摘要
Dayuan fluor deposit is located on the south-east leg of Jinjiling anticline, Wuchuan mercury deposit belt in Dejiang County. The ore body occupies in the first dolomitized limestone of the Qingxudong Formation in low Cambrian, the occurrence layer is special, the mineral combination is simple and the quality is high. By primary research, the formation of fluor deposit has relationship with the activities of low temperature thermal brine, and it’s controlled by tensile fracture, lithofacies ancient geology and rock association strictly. The strata-binding is obviously and the mineralization is in Yanshan stage.