The Anle fluorite deposit in Wangmo,Guizhou Province is in the tensional fault structure of Upper Permian Wujiaping Formation and the"silicified erosion variant"at the bottom of Triassic Luolou Formation.On the basis of summarizing the geological characteristics of the fluorite deposit in this area,the formation period,spatial distribution law,ore-forming material source,interface and tectonic metallogenetic regularity are analyzed.The results show that the fluorite deposit in this area is related to geological conditions such as stratigraphic lithology(interface),structure and alteration of surrounding rock,and is an epithermal deposit.This paper summarizes 4 prospecting signs in order to provide reference for a new round of prospecting breakthrough strategic action for fluorite ore prospecting.
metallogenic regularityprospecting indicatorfluorite oreAnle in Wangmo
维普
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