收稿日期: 2020-09-01
修回日期: 2021-01-26
网络出版日期: 2021-05-28
基金资助
国家自然科学基金项目“山东招远—平度断裂带夏甸金矿深部成矿特征研究”(41572068);国家重点研发计划项目“胶西北地区深部构造格架研究——依托于深部反射地震”(2016YFC0600107-5);国家公益性行业科研专项“胶东招平断裂带深部特征与金矿成矿过程研究”(201511029);“招平断裂带中段深部金矿成矿理论、找矿方法与成矿预测”(2017CXGC1605);山东省泰山学者建设工程专项联合资助
Genesis of Xiadian Gold Deposit in Jiaodong:Evidence from Fluid Inclusions and Isotopes
Received date: 2020-09-01
Revised date: 2021-01-26
Online published: 2021-05-28
为探讨夏甸金矿床成矿流体性质和来源,对该金矿-740~-820 m中段Ⅶ号矿体金矿石样品进行包裹体和S、H、O稳定同位素测定。夏甸金矿包裹体类型以富液体包裹体为主,其次为富气体包裹体和H2O-CO2三相包裹体,气液相比一般为10%~15%,
李逸凡 , 李洪奎 , 韩学林 , 耿科 , 张玉波 , 陈国栋 . 胶东夏甸金矿床成因:流体包裹体及同位素证据[J]. 黄金科学技术, 2021 , 29(2) : 184 -199 . DOI: 10.11872/j.issn.1005-2518.2021.02.157
Gold ore fluid inclusions and S, H and O stable isotopes from -740~-820 m middle section of ore body VII in Xiadian gold deposit were measured to study the ore-forming fluid properties and sources.The fluid inclusions are mainly liquid rich inclusions, followed by gas rich inclusions and H2O-CO2 three-phase inclusions. The gas-liquid ratio is generally 10~15, and
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