咨询与建议

看过本文的还看了

相关文献

该作者的其他文献

文献详情 >U-Pb and Re-Os Geochronology o... 收藏
U-Pb and Re-Os Geochronology of the Tongcun Molybdenum Depos...

U-Pb and Re-Os Geochronology of the Tongcun Molybdenum Deposit and Zhilingtou Gold-Silver Deposit in Zhejiang Province,Southeast China,and Its Geological Implications

作     者:Qingdong ZENG Yongbin WANG Song ZHANG Jianming Liu Kezhang QIN Jinhui YANG Weidong SUN Wenjun Qu 

作者单位:Key Laboratory of Mineral ResourcesInstitute of Geology and GeophysicsChinese Academy of Sciences Key Laboratory of Isotope Geochronology and GeochemistryChinese Academy of Sciences Re-Os Laboratory of National Research Center of GeoanalysisChinese Academy of Geological Sciences 

会议名称:《中国科学院地质与地球物理研究所2013年度(第13届)学术年会》

会议日期:2014年

学科分类:070902[理学-地球化学] 0709[理学-地质学] 07[理学] 

基  金:funded by the Foundation for Major Projects(the Geodynamics and Prospecting Exploration Demonstration for the Mesozoic Metallogenesis in Southeast China)of Innovation Program established by the Chinese Academy of Sciences 

关 键 词:Mesozoic Re-Os dating U-Pb dating Zhejiang Province 

摘      要:Mesozoic ore deposits in Zhejiang Province,Southeast China,are divided into the northwestern and southeastern Zhejiang metallogenic belts along the Jiangshan-Shaoxing *** metal ore depos- its found in these belts are epithermal Au-Ag deposits,hydrothermal-vein Ag-Pb-Zn deposits, porphyry-skarn Mo(Fe)deposits,and vein-type Mo *** is a close spatial-temporal relationship between the Mesozoic ore deposits and Mesozoic volcanic intrusive *** U-Pb dating of the ore-related intrusive rocks and molybdenite Re-Os dating from two typical deposits(Tongcun Mo deposit and Zhilingtou Au-Ag deposit)in the two metallogenic belts show the early and late Yanshanian ages for *** U-Pb data of zircons from the Tongcun Mo deposit and Zhilingtou Au-Ag deposit indicate that the host granitoids crystallized at 169.7±9.7 Ma(2σ)and 113.6±1 Ma(2σ),***-Os analysis of six molybdenite samples from the Tongcun Mo deposit yields an isochron age of 163.9±1.9 Ma(2σ).Re-Os analyses of five molybdenite samples from the porphyry Mo orebodies of the Zhilingtou Au-Ag deposit yield an isochron age of 110.1±1.8 Ma(2σ).Our results suggest that the metal mineralization in the Zhejiang Province,southeast China formed during at least two stages,i.e.,Middle Jurassic and Early Cretaceous,coeval with the granitic magmatism.

读者评论 与其他读者分享你的观点

用户名:未登录
我的评分