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西藏墨竹工卡县洞中拉铅锌矿床S、Pb同位素组成及成矿物质来源

刘婷婷 唐菊兴 刘鸿飞 张金树 崔晓亮 高一鸣

现代地质2011,Vol.25Issue(5):869-876,8.
现代地质2011,Vol.25Issue(5):869-876,8.

西藏墨竹工卡县洞中拉铅锌矿床S、Pb同位素组成及成矿物质来源

Sulfur and Lead Isotope Composition and Tracing for Sources of Ore-forming Materials in the Dongzhongla Pb-Zn Deposits in Mozhugongka County, Tibet

刘婷婷 1唐菊兴 1刘鸿飞 2张金树 3崔晓亮 3高一鸣1

作者信息

  • 1. 成都理工大学地球科学学院,四川成都610059
  • 2. 中国地质科学院矿产资源研究所,北京100037
  • 3. 西藏自治区地质矿产勘查开发局,西藏拉萨851400
  • 折叠

摘要

Abstract

In order to discuss the ore-forming material sources of the Dongzhongla Pb-Zn deposits and study the metallogenic mechanism, we analyzed the sulfur and lead isotope from the orebody, discussed the changing regularity and significance. The results show that the δ34S values of the six metal sulfides vary from 2. 2%c to 4. 8%e, and that the sulfur isotope composition is stable. The temperatures calculated from sulfide-paras show that the deposits are the middle-low temperature deposits. The 206Pb/204Pb,207Pb/204Pb and 208Pb/204 Pb ratios of 6 sulfide samples of orebody vary in ranges of 18.628 0 - 18.629 6, 15. 698 - 15. 699 9, 39.0775 -39. 082 4, with the average values of 18. 628 7, 15. 699 02 and 39. 079 37, respectively. The results of sulfur and lead isotope show that the ore-forming materials of Dongzhongla Pb-Zn deposits came from the Permian volcanic sedimentary rock and late Yanshan period granite.

关键词

S、Pb同位素/成矿物质来源/洞中拉铅锌矿床/热液矿床/δ34S值/上地壳物质

Key words

sulfur and lead isotope/ ore-forming material source/ Dongzhongla lead-zinc deposits/ hydrothermal deposit/ δ34S value/ upper crust material

分类

天文与地球科学

引用本文复制引用

刘婷婷,唐菊兴,刘鸿飞,张金树,崔晓亮,高一鸣..西藏墨竹工卡县洞中拉铅锌矿床S、Pb同位素组成及成矿物质来源[J].现代地质,2011,25(5):869-876,8.

基金项目

中国地质调查局项目"念青唐古拉地区成矿条件研究与找矿靶区优选"(1212010818089) (1212010818089)

国家科技支撑项目"中西部大型矿产基地综合勘查技术与示范"(2006BAB01A01). (2006BAB01A01)

现代地质

OA北大核心CSCDCSTPCD

1000-8527

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