摘要
在矿床地质研究的基础上,从矿物包裹体的显微岩相学、均一化温度、成分、含盐度和H、0、C稳定同位素组成方面,探讨了水口山Pb─Zn─Au矿田含矿流体的性质、来源及其环流历程。含矿流体系由岩浆期后热液和地下水混合而成。对于水口山矿区而言,岩浆热液起着主导作用;对于康家湾矿区而言,岩浆期后热液和地下水热液均起着重要作用。热液成矿期从早到晚,随着温度和含盐度的逐渐降低,地下水中雨水/地层卤水的比值逐渐增大。含矿流体的环流历程经历了5个阶段。
Based on investigation of ore deposit geology, a Systematic Study has been made on H,O,C Stable isotopic compositions and mineral inclusions from their micrography,homogenization temperature,composition, salinity. The ore─bearing fluid is constrained in the Shuikoushan Pb─Zn─Au ore field about its nature,source and convection path.It is a mixture district is dominated by the former.In the Kangjiawan ore district,however,both kinds of fluids are important.With evolution of the hydrothermal metallogenesis,when temperature and salinity are progressively decreased, ratio of meteoric water/ stratum brine in the subsurface water is increased.Convection of the ore─bearing fluid saw 5 periods.
出处
《大地构造与成矿学》
EI
CAS
CSCD
1994年第3期209-209,共1页
Geotectonica et Metallogenia
基金
中科院院长基金
武汉分院择优支持项目
关键词
含矿流体
铅-锌-金
矿田
矿物包体
ore─bearing fluid,mineral inclusion, stable isotope, Shuikoushan Pb─Zn─Au ore field