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紫金山铜金矿黄铁矿碎裂结构特征及其地质意义 被引量:4

Characteristics of fragmentation pyrite and its geological implication in Zijinshan Cu-Au Deposit
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摘要 紫金山铜金矿黄铁矿的碎裂结构具有三种赋存状态,主要运用电子探针(EPMA)对其进行微区分析,进而探讨碎裂结构黄铁矿的特征及其地质意义。通过研究得出以下主要结论:1)本矿碎裂结构黄铁矿的三种赋存状态:破碎程度一般,颗粒较大;破碎程度大,颗粒细小;碎裂结构与粒状结构黄铁矿共生。黄铁矿的破碎程度越大,颗粒越细小,含金性越大,且黄铁矿中金的赋存状态为纳米级颗粒金;2)碎裂结构黄铁矿是亏铁富硫型的,从浅部到深部,亏铁程度与富硫程度逐渐减弱,黄铁矿的Co-Ni图解,说明其是火山—热液成因,其形成与早期隐爆作用有关;3)碎裂结构黄铁矿的主要微量元素有Cu、Co、Ni、Pb、Zn、Au、Ag、As、Sb、Se、W、Sn等,从浅部到深部,碎裂结构黄铁矿的微量元素Sn含量明显增加;元素W、Au、Zn、Ag、Pb都有逐渐降低的趋势;Ni含量也逐渐降低,但是靠近铜矿体,其含量有所增加;越接近铜矿体,Cu与S的含量增加,而Fe的含量降低,体现了紫金山铜金矿床的成矿流体是火山热液(形成于燕山晚期,富含Cu、Au、Pb、Zn等成矿元素)与紫金山复式花岗岩岩体(形成于燕山早期,具有W、Sn、Mo、Bi等矿化特征)的叠加。 Fragmentation structure of pyrites has three kinds of states in Zijinshan Cu-Au deposit,this paper investigated its characteristics and geological implication by the micro area analysis on EPMA.Though the study,we make the following conclusion:1)The three occurrence fragmentation structure pyrites in this deposit:General fragmentation,larger particles;large degree of fragmentation,tiny particles;fragmention pyrite co-occurrence with granular structure pyrite.The larger degree of fragmentation pyrite,the smaller particles,the greater contents of the gold,the occurrence of gold in pyrite is nanoscale particles gold.2)The fractured pyrite is iron-deficiency,sulfur-rich type.The degree of iron-deficiency sulfur-rich gradually weakened from shallow to deep part;The Co-Ni diagram of pyrite show that it is the volcano-hydrothermal origin and relevant to early cryptoexplosion.3)The main trace elements of fragmentation pyrite included Cu、Co、Ni、Pb、Zn、Au、Ag、As、Sb、Se、W、Sn and so on.From shallow to deep part,the content of Sn was increased;the content of W、Au、Zn、Ag and Pb gradually decreased.The content of Ni also decreased,but increased near the copper body.Approaching to copper body,the contents of Cu and S increased,while the content of Fe decreased.It presented that the ore-forming fluid is rich in ore elements such as Cu,Au,Pb,Zn,etc.The volcanic hydrothermal fluid with ore-forming elements superimposed on the early Yanshan Zijinshan composite granite pluton which is mineralized with W,Sn,Mo,Bi,etc.
出处 《有色金属(矿山部分)》 2015年第1期36-42,共7页 NONFERROUS METALS(Mining Section)
基金 国家自然科学基金(41072067)
关键词 紫金山铜金矿 黄铁矿 碎裂结构 电子探针 地质意义 Zijinshan Cu-Au deposit pyrite fragmentation structure electron probe geological implication
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