• 首页
  • 关于本刊
  • 编委会
  • 在线投稿
  • 过刊浏览
  • 欢迎订阅
  • 相关下载
  • 基本常识
  • English
:2021,Vol.>>Issue(6):1214-1229

河北涞源大湾锌钼矿床锆石U-Pb和辉钼矿Re-Os年龄及其地质意义
河北地质大学 河北省战略性关键矿产资源重点实验室, 河北 石家庄 050031;河北省地质工程勘查院, 河北 保定 071051;中国地质大学 科学研究院, 北京 100083
Zircon U-Pb and molybdenite Re-Os dating of Dawan Zn-Mo deposit in Laiyuan County of Hebei Province and its geological significance
TIAN Lin,ZHANG Zhi-yuan,WANG Zhi-min,DING Zhao-yue,LI Tian-qi,LU Hong-peng,AN Yue-hui,HU Hua-bin,XIE Gui-qing
(Hebei Key Laboratory of Strategic Critical Mineral Resources, Hebei GEO University, Shijiazhuang 050031, Hebei, China;Hebei Geological Engineering Exploration Institute, Baoding 071051, Hebei, China;Institute of Earth Sciences, China University of Geosciences, Beijing 100083, China)
本文二维码信息
码上扫一扫!

摘要
图/表
参考文献
相似文献

摘要点击次数: 407   全文下载次数: 243   点此下载全文
投稿时间:2021-07-06   修订日期:2021-08-24      网络发布日期:2022-01-11
中文摘要:大湾斑岩-矽卡岩型锌钼矿床地处太行山北段成矿带中,是该段重要的金属矿床之一。五台群板峪口组和长城系高于庄组为主要赋矿围岩,锌钼矿体主要赋存在流纹斑岩体内及斑岩与围岩接触部位。文章对大湾矿床内2件赋矿流纹斑岩进行LA-ICP-MS锆石U-Pb年代测定,获得206Pb/238U年龄加权平均值分别为(137.1±0.9)Ma(MSWD=0.56,n=24)和(136.8±1.2)Ma(MSWD=0.40,n=22);对矿区4件辉钼矿样品进行Re-Os定年,得到加权平均年龄为(136.5±1.0)Ma,等时线年龄为(136.1±2.3)Ma,在误差范围内成岩成矿时代一致,显示大湾锌钼矿床形成于早白垩世。大湾矿床中辉钼矿的w(Re)为5.816~16.484μg/g,反映了矿床成矿物质来源具有壳幔混合特征。区内流纹斑岩和蚀变体系为进一步找矿勘查的有利标志。
Abstract:The Dawan porphyry-skarn Zn-Mo deposit is one of important metal deposits in the northern Taihang Mountain metallogenic belt. The Banyukou Formation of Wutai Group and the Gaoyuzhuang Formation of Changcheng System are the main country rocks of the mineralization related intrusive rocks. The Zn-Mo ore body mainly occurs in rhyolite porphyry and the contact zones of rhyolite porphyry and its country rocks. In this paper, the LA-ICP-MS zircon U-Pb analysis of the two rhyolite porphyry samples from the Dawan deposit yielded the weighted 206Pb/238U mean ages as(137.1±0.9)Ma(MSWD=0.56, n=24) and(136.8±1.2)Ma(MSWD=0.40, n=22), respectively. Re-Os dating of four molybdenite samples show that the weighted mean age and isochron age are(136.5±1.0)Ma and(136.1±2.3)Ma, respectively, which indicates that the Dawan deposit was formed in the Early Cretaceous. The w(Re) of molybdenite vary in the range of 5.816~16.484 μg/g, showing that they were derived from mixed crust and mantle sources. Rhyolite porphyry and porphyry-related alteration system in the Dawan deposit are the useful indication for prospecting and exploration of the same style mineralization in the region.
文章编号:    
中图分类号:     
文献标志码:

基金项目:河北省自然科学基金(编号:D2020403060)、国家自然科学基金(编号:41925011)、河北省地质矿产勘查开发局项目(编号:454-0502-JBN 0HDV)联合资助
引用文本:
田林,张志远,王志敏,丁照月,李天琦,卢鸿鹏,安跃辉,胡华斌,谢桂青.2021.河北涞源大湾锌钼矿床锆石U-Pb和辉钼矿Re-Os年龄及其地质意义[J].矿床地质,40(6):1214~1229
TIAN Lin,ZHANG Zhi-yuan,WANG Zhi-min,DING Zhao-yue,LI Tian-qi,LU Hong-peng,AN Yue-hui,HU Hua-bin,XIE Gui-qing.2021.Zircon U-Pb and molybdenite Re-Os dating of Dawan Zn-Mo deposit in Laiyuan County of Hebei Province and its geological significance[J].Mineral Deposits40(6):1214~1229
图/表
您是第227500182位访问者  京ICP备05032737号-5  京公网 安备110102004559
版权所有:《矿床地质》编辑部
主管单位:中国科学技术协会 主办单位:中国地质学会矿床地质专业委员会 中国地质科学院矿产资源研究所
地  址: 北京市百万庄大街26号 邮编:100037 电话:010-68327284;010-68999546 E-mail: minerald@vip.163.com
本系统由北京勤云科技发展有限公司设计 
手机扫一扫