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黑龙江三道湾子碲金矿床物质组成及成因意义

韩思宇 翟德高 刘家军 吕军 吴胜华 杨隆勃

矿床地质2011,Vol.30Issue(5):855-866,12.
矿床地质2011,Vol.30Issue(5):855-866,12.

黑龙江三道湾子碲金矿床物质组成及成因意义

Mineral assemblage of Sandaowanzi tellurium-gold deposit in Heilongjiang Province and its genetic significance

韩思宇 1翟德高 2刘家军 1吕军 2吴胜华 1杨隆勃2

作者信息

  • 1. 中国地质大学地球科学与资源学院,北京100083
  • 2. 中国地质大学地质过程与矿产资源国家重点实验室,北京100083
  • 折叠

摘要

Abstract

The Sandaowanzi tellurium-gold deposit is a typical telluride-gold deposit in northern Heilongjiang Province. The ore deposit located in the central section of the Da Hinggan Mountains. Microscope observation and electron microprobe analyses of mineral assemblages of this deposit reveal that 6 different kinds of tellurides such as petzite, sylvanite, calaverite, hessite and altaite are existent in ores of this ore deposit. Lots of native gold occurring in veins of quartz and petzite or coexistent with tellurides were also found in this ore deposit. EP-Matest shows that Au possesses 85.64%~93.41% and Ag possesses 6.17%~ 13.48% in native gold, which can be classified as Ag-bearing native gold with gold fineness of 864-938. Tellurium could easily replace sulfur in middle-low temperature, making tellurium dispersed in lattice of sulfides in the isomorphous form, whereas under high tellurium fugacity conditions, tellurium could easily coexist with Au and Ag to form a number of tellurides.

关键词

地质学/碲金矿床/碲化物/自然金/三道湾子/黑龙江

Key words

geology/tellurium-gold deposit/tellurides/native gold/Sandaowanzi/Heilongjiang

分类

天文与地球科学

引用本文复制引用

韩思宇,翟德高,刘家军,吕军,吴胜华,杨隆勃..黑龙江三道湾子碲金矿床物质组成及成因意义[J].矿床地质,2011,30(5):855-866,12.

基金项目

本文为国家自然科学基金(40973035) (40973035)

教育部长江学者和创新团队发展计划(IRT0755) (IRT0755)

高等学校学科创新引智计划(B07011)和中国地质调查局“我国三稀金属资源战略调查”项目(编号1212011120354)的部分研究成果 (B07011)

矿床地质

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