摘要
为查明抱伦金矿金的赋存状态,在矿相学观察的基础上,开展毒砂成分电子探针微区测试。结果表明:毒砂中金质量分数高达0. 75%,但分布不均。Fe质量分数在30. 5%~36. 2%,As质量分数在39. 8%~48. 0%,S质量分数在16. 3%~22. 6%,As摩尔分数为29. 1%~34. 9%。金与其他元素无明显的相关性,说明晶格内的金对金含量影响甚微,金主要以包体的形式存在于毒砂中。毒砂形成条件为毒砂和磁黄铁矿组合与毒砂和斜方砷铁矿组合的相过渡条件下,成矿温度在350℃左右。该研究证实抱伦金矿属于中-高温热液矿床。
This paper describes electron probe microanalysis of arsenopyrite composition performed based on mineralogical observation so as to determine the occurrence of gold in Baolun gold deposit.The results show that arsenopyrite has the gold content of up to 0.75%,but with uneven distribution;the mass fractions are 30.5%-36.2%,39.8%-48.0%,16.3%-22.6%and 29.1%-34.9%respectively for Fe,As,S and As;and the absence of an obvious correlation between gold and other elements indicates that the gold in the lattice has little influence on gold content,meaning that gold occurs in arsenopyrite mainly as inclusion;arsenopyrite forms at the mineralization temperature of about 350℃during the phase transformation of arsenopyrite and pyrite assemblage and arsenopyrite and lollingite assemblage.The research confirms the Baolun gold deposit belongs to meso-hypothermal deposit.
作者
于亮亮
许德如
Yu Liangliang;Xu Deru(School of Mining Engineering,Heilongjiang University of Science & Technology,Harbin 150022,China;State Key Laboratory of Nuclear Resources & Environment,East China University of Technology,Nanchang 330013,China)
出处
《黑龙江科技大学学报》
CAS
2019年第1期115-118,共4页
Journal of Heilongjiang University of Science And Technology
基金
黑龙江省自然科学基金项目(QC2017035)
关键词
金赋存状态
成矿温度
毒砂
电子探针
抱伦金矿
gold occurrence
metallogenic temperature
arsenopyrite
electron probe
Baolun gold deposit