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紫金山金铜矿二元铜硫化物成分特点的初步研究

刘羽 刘文元 王少怀

矿床地质2011,Vol.30Issue(4):735-741,7.
矿床地质2011,Vol.30Issue(4):735-741,7.

紫金山金铜矿二元铜硫化物成分特点的初步研究

Preliminary compositional investigation of binary Cu sulfidesfrom Zijinshan Au-Cu deposit

刘羽 1刘文元 1王少怀1

作者信息

  • 1. 福建省矿产资源重点实验室,福州大学紫金矿业学院,福建福州350108
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摘要

Abstract

In this paper, the chemical composition of some binary Cu sulfides from highly sulfidized epithermal Zijin-shan Au-Cu deposit was investigated, and mineral phases in the ores were determined with electron microprobe analysis, X-ray diffraction and vibrational spectroscopy. Djurleite (Cu1.97S)and yarrowite(Cu1.25S)from this ore deposit were recognized for the first time. In addition to the replacement of digenite (Cu1.80S) by covellite (Cu1.01S), some covellite was replaced by digenite and anilite (C111.75S). These phenomena imply that these Cu sulfides were formed contemporarily from the same hydrothermal solution, but under different oxidization-deoxi-dization conditions. The formation of these minerals resulted from the alteration of the earlier primary sulfides by Cu-rich hydrothermal solutions.

关键词

矿物学/二元铜硫化物/显微分析/紫金山金铜矿

Key words

mineralogy/binary Cu sulfides/microanalysis/Zijinshan Au-Cu deposit

分类

天文与地球科学

引用本文复制引用

刘羽,刘文元,王少怀..紫金山金铜矿二元铜硫化物成分特点的初步研究[J].矿床地质,2011,30(4):735-741,7.

基金项目

本文得到福建省自然科学基金(编号:2009J01215、2009J01216)和国家科技支撑计划重点项目(编号:2009BAB43B00)联合资助 (编号:2009J01215、2009J01216)

矿床地质

OA北大核心CSCDCSTPCD

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