摘要
对浙江武义盆地萤石矿的研究表明，其成矿物质来自围岩，介质为大气降水，热源来自构造－岩浆活动，成矿温度为１３０℃±。矿液在渗透、迁移过程中从围岩中吸取矿质，又在迁移演化过程中，由于物理化学条件的变化。
The researchs on the fluorite deposits of Wuyi basin in Zhejiang show that the ore forming matter of the deposits comes from the wall rocks, the medium is meteoric water, the thermal source originates from tectonic magmatic activities and the mineralization temperature is 130℃±. The ore solution absorbs mineral matter from the wall rocks in the process of permeation and migration. And in the process of migration and evolution, the ore solution forms epithermal fluorite deposits in favourabe environment of geological structure because of the changes in physical and chemical conditions.
出处
《成都理工学院学报》
CSCD
1996年第4期46-49,共4页
Journal of Chengdu University of Technology
