摘要
赣西卡林型金矿受地层层位及构造控制 ,呈层状、似层状及透镜状产出。规模为中小型。金矿化与硅化、黄铁矿化及有机碳关系密切。主成矿温度平均 150℃左右 ,成矿压力为 2 4 7× 10 5Pa～ 60 8× 10 5Pa。
WT5BZ]Carlin type Gold deposit in western jiangxi is controlled by stratohorizon and structure and it occur as strataform, strataform like and lenticular in middle and small type scale. Gold mineralion is closely reated silicification, pyrite mineralization and organic carbon. Main mineralization temperature is about 150℃ and the pressure is 247×10 5pa～608×10 5pa. Ore fluid is hot brine dominated by atmospheric water. [WT5HZ]
出处
《矿产与地质》
2000年第6期365-370,共6页
Mineral Resources and Geology
基金
原中国有色金属工业总公司科研项目!项目编号 94- D- 4
