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利用铅同位素研究山东邹平王家庄铜矿地气物质来源
引用本文:徐洋,汪明启,高玉岩,等.利用铅同位素研究山东邹平王家庄铜矿地气物质来源[J].物探与化探,2014(1):23-27.
作者姓名:徐洋  汪明启  高玉岩  
作者单位:[1]中国地质大学地球科学与资源学院,北京100083 [2]中铁资源地质勘查有限公司,北京100074
基金项目:国家高科技研究发展计划(863)项目(2006AA06Z102)
摘    要:铅同位素示踪是采用铅同位素作为示踪剂,根据有关岩石、矿物的铅同位素组成和它们之间的关系判断成矿物质来源。笔者利用铅同位素示踪地气物质来源,采用ICP-MS测试方法,对山东邹平王家庄斑岩铜矿区矿石、围岩、土壤等介质的铅同位素组成与地气样品铅同位素特征进行对比,发现矿体上方地气异常样品铅同位素组成与矿石中铅同位素组成基本一致,表明地气异常样品中的铅主要来自深部矿体,且捕集剂空白和其他影响因素对地气异常样品中铅的干扰较小,其铅同位素组成更接近于矿石。

关 键 词:铅同位素示踪  地气测量  斑岩铜矿  邹平王家庄

TRACING THE SOURCE OF GEOGAS MATERIALS WITH THE LEAD ISOTOPE METHOD IN THE WANGJIAZHUANG COPPER ORE DEPOSIT OF ZOUPING,SHANDONG PROVINCE
XU Yang,WANG Ming-qi,GAO Yu-yan,OU Yang-hui.TRACING THE SOURCE OF GEOGAS MATERIALS WITH THE LEAD ISOTOPE METHOD IN THE WANGJIAZHUANG COPPER ORE DEPOSIT OF ZOUPING,SHANDONG PROVINCE[J].Geophysical and Geochemical Exploration,2014(1):23-27.
Authors:XU Yang  WANG Ming-qi  GAO Yu-yan  OU Yang-hui
Institution:1 ( 1. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China ; 2. China Railway Resources Exploration Co., Ltd. Beijing 100074, China)
Abstract:Lead isotopic tracing is a method for identifying the ore-forming materials according to the lead isotope ratios of rocks, minerals and their relationships. This method was used to trace the geogas components of the Wangjiazhuang copper deposit in Zouping, Shandong Province. A comparison of the lead isotope ratios of ores, wall-rocks and soil with those of geogas samples by using ICP-MS analysis shows that the lead isotopic composition of abnormal geogas samples is in accordance with that of ores, suggesting that the lead in abnormal geogas samples comes from deep-buried ore bodies.
Keywords:lead isotope tracing  geogas technique  porphyry copper deposit  Wangjiazhuang in Zouping
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