江西永丰南坑萤石矿床地质特征控矿地质条件及成因

The Geological Charecteristics Controlled Geological Conditions and Geneses of Nankeng Fluorite Depasit in Yongfeng Jiangxi Province

根据产于花岗岩断裂破碎带中的脉状萤石矿床地质特征,控矿地质条件及地下水热液成矿作用研究,表明产于花岗岩断裂破碎带中的脉状萤石矿床并不属于岩浆期后热液矿床。

According to the geological characteristies of Nankeng vein fluorite deposit located in fractured zone of granite, the confrolled geological conditions and groundwater hydro -thermal mineralizafion are discussed in this paper. The study show that the mineralizafian of vein fluorite deposit located in tractured zone of granite is not belong to post - magmafic hyrotherinal deposit.