摘要
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.
出处
《西南工学院学报》
1993年第4期55-63,共9页
Journal of Southwest China Institute of Technology
关键词
花岗岩
萤石矿床
地质特征
成矿
granife fluorite deposit characteristis geneses