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有色金属(矿山部分):2018,70(6):54-62
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福建紫金山铜矿床深部铜硫矿物空间分布特征初探
阮诗昆
(紫金矿业集团股份有限公司)
Preliminary study on spatial distribution characteristics of copper sulfide minerals in deep Zijinshan copper deposit, Fujian province
Ruan Shikun
(Zijin Mining Group CO.,LTD.)
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投稿时间:2018-05-22    修订日期:2018-06-16
中文摘要: 紫金山铜矿床深部铜硫矿物种类丰富,通过自上而下针对铜硫二元体系矿物系统采样,经手标本观察后利用矿相显微镜和电子探针分析,共检测出5种Cu-S体系矿物,包括蓝辉铜矿、铜蓝、斜方蓝辉铜矿、吉硫铜矿和久辉铜矿,含矿层Cu-S体系矿物组合自上而下分为4带,分布标高自300~-130m,主要铜矿物为蓝辉铜矿、铜蓝、斜方蓝辉铜矿,次要铜矿物为吉硫铜矿和久辉铜矿;通过对岩性和铜硫矿物组合的分析,深部铜矿体为可分为2层铜矿体,上段铜矿体铜硫矿物组合类型为铜蓝-斜方蓝辉铜矿-蓝辉铜矿,下段铜矿体铜硫矿物主要为斜方蓝辉铜矿;矿床深部随着标高的降低,硫逸度和氧逸度逐渐上升,暗示着矿床深部具有较好的斑岩型矿床找矿远景。
Abstract:Cu-S minerals in deep Zijinshan Copper deposit are abundant, by sampling Cu-S series minerals systematically from top to bottom, 5 kinds of Cu-S system minerals were detected by means of ore microscope and electron probe after hand specimen observation, including digenite, covellite, anilite, geerite and djurleite. Cu-S series minerals of the ore bearing layer is divided into 4 bands from top to bottom whose distribution elevation was from 300m to -130m. The main copper minerals were digenite, covellite, anilite, The secondary copper minerals were geerite and djurleite. The deep copper ore body can be divided into 2 layers through the analysis of lithology and copper sulfide minerals, Cu-S series minerals of upper ore-body was covellite-anilite-digenite and lower ore-body was mainly anilite. In deep part of deposit, the sulfur fugacity and oxygen fugacity gradually increase with the decrease of the elevation, implying that there would be a good prospect for porphyry deposit prospecting.
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基金项目:国家重点研发计划-穿透性地球化学勘查技术(2016YFC0600600)
Author NameAffiliationE-mail
Ruan Shikun Zijin Mining Group CO.,LTD. ruanshikun@126.com 
引用文本:
阮诗昆.福建紫金山铜矿床深部铜硫矿物空间分布特征初探[J].有色金属(矿山部分),2018,70(6):54-62.
Ruan Shikun.Preliminary study on spatial distribution characteristics of copper sulfide minerals in deep Zijinshan copper deposit, Fujian province[J].NONFERROUS METALS(Mining Section),2018,70(6):54-62.

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