ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
江西九瑞地区东雷湾矽卡岩型铜多金属矿床锆石U-Pb和辉钼矿Re-Os年龄及其地质意义
  
关键词:metallogenetic setting  zircon U-Pb age  molybdenite Re-Os age  skarn copper-polymetallic deposit  Dongleiwan mining area  Jiujiang–Ruichang ore concentration area
基金项目:国家十二五科技支撑计划课题(编号: 2009BAB43B03; 2011BAB04B03);国家专项“深部探测技术与实验研究”(编号: SinoProbe-03-06);国土资源部公益性行业科研专项(编号: 201311166(SinoProbe-03-07))
作者单位E-mail
贾丽琼 中国地质大学(北京)地球科学与资源学院, 地质过程与矿产资源国家重点实验室
中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室 
jialiqiong@126.com 
杨丹 中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室 yangd_2013@163.com 
徐文艺 中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室  
吕庆田 中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室  
杨竹森 中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室  
莫宣学 中国地质大学(北京)地球科学与资源学院, 地质过程与矿产资源国家重点实验室  
王梁 中国地质大学(北京)地球科学与资源学院, 地质过程与矿产资源国家重点实验室
武警黄金地质研究所 
 
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摘要:
Zircon U-Pb and Molybdenite Re-Os Dating of the Dongleiwan Skarn Cu Polymetallic Deposit in the Jiujiang–Ruichang Ore Concentration Area of Jiangxi Province and Its Geological Significance
      The Dongleiwan skarn Cu-Mo-Au polymetallic deposit is located in northwestern Jiujiang–Ruichang ore concentration area. U-Pb LA-MC-ICP MS dating of zircons from Dongleiwan granodiorite porphyry yielded an age of (142.24±0.52) Ma. Six molybdenite samples separated from quartz sulfides in Dongleiwan skarn orebodies were used for Re-Os dating and the model ages obtained range from (144.8±3.1) Ma to (147.1±2.4) Ma, with weighted average (146.12±0.97) Ma and isochron age (143.3±5.2) Ma. These ages suggest that the mineralization in the Dongleiwan skarn copper-polymetallic deposit was genetically associated with the granodiorite porphyry, and the rock-forming and ore-forming processes were quite consistent with each other. The Re content of molybdenite indicates that the ore-forming materials were derived from the mantle and the crust. These data show that ages of rock body and ore body in the Dongleiwan deposit are almost identical with ages of other typical rock masses and deposits in the Jiujiang–Ruichang ore concentration area, and even quite close to ages of typical Cu-polymetallic deposits in such areas as Tongling, Anqing and part of southeast Hubei along the Middle–Lower Yangtze River metallogenic belt. Based on regional tectonic evolution, it is inferred that the Dongleiwan deposit was formed in the transition period from EW-striking Indosinian tectonic domain to NE-striking Paleo-Pacific tectonic domain.
JIA Li-qiong,YANG Dan,XU Wen-yi,LÜ Qing-tian,YANG Zhu-sen,MO Xuan-xue,WANG Liang.2015.Zircon U-Pb and Molybdenite Re-Os Dating of the Dongleiwan Skarn Cu Polymetallic Deposit in the Jiujiang–Ruichang Ore Concentration Area of Jiangxi Province and Its Geological Significance[J].Acta Geoscientica Sinica,36(2):177-186.
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