摘要
文章对望谟打岩背斜萤石矿床地质特征及流体包裹体特征进行了初步研究显示,萤石矿体主要赋存于吴家坪组地层及硅质蚀变岩中,萤石流体包裹体均一温度范围在130℃~180℃之间,应属地下热水(热卤水)充填型矿床。
The preliminary research in geological characteristics and fluid inclusions of Wangmo Dayan anticline fluorite ore deposit showed that,fluorite ore bodies mainly occur in the Wujiaping formation and alteration siliceous rocks,and homogenization temperature of fluorite fluid inclusions in the range of 130℃ -180℃, should belong to the underground hot water （hot brine） filling deposit.
作者
蒋良兵
JIANG Liang-bing(Guizhou Geological Survey, Guiyang, Guizhou 550000, Chin)
出处
《企业技术开发》
2017年第10期45-46,共2页
Technological Development of Enterprise
关键词
萤石矿
地质特征
打岩背斜
望谟
fluorite
Geological characteristics
Dayan anticline
Wangmo
