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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

徐洋 汪明启 高玉岩 欧阳辉

物探与化探Issue(1):23-27,5.
物探与化探Issue(1):23-27,5.DOI:10.11720/j.issn.1000-8918.2014.1.04

利用铅同位素研究山东邹平王家庄铜矿地气物质来源

TRACING THE SOURCE OF GEOGAS MATERIALS WITH THE LEAD ISOTOPE METHOD IN THE WANGJIAZHUANG COPPER ORE DEPOSIT OF ZOUPING, SHANDONG PROVINCE

徐洋 1汪明启 1高玉岩 2欧阳辉1

作者信息

  • 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
  • 折叠

摘要

Abstract

Lead isotopic tracing is a method for identifying the ore-forming materials according to the lead isotope ratios of rocks, min-erals 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.

关键词

铅同位素示踪/地气测量/斑岩铜矿/邹平王家庄

Key words

lead isotope tracing/geogas technique/porphyry copper deposit/Wangjiazhuang in Zouping

分类

天文与地球科学

引用本文复制引用

徐洋,汪明启,高玉岩,欧阳辉..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):23-27,5.

基金项目

国家高科技研究发展计划(863)项目 ()

物探与化探

OACSCDCSTPCD

1000-8918

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