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甘肃大店沟金矿床中脆硫锑铅矿的发现与成矿启示

樊荣 司明扬 刘家军 张斌 曹瑞荣 来召 艾忠林 于谦 杜佰松

现代地质2026,Vol.40Issue(4):1023-1033,11.
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现代地质2026,Vol.40Issue(4):1023-1033,11.DOI:10.19657/j.geoscience.1000-8527.202508260034

甘肃大店沟金矿床中脆硫锑铅矿的发现与成矿启示

Discovery of Jamesonite from the Dadiangou Gold Deposit,Gansu Province and Its Genetic Significance

樊荣 1司明扬 2刘家军 2张斌 2曹瑞荣 1来召 1艾忠林 1于谦 1杜佰松3

作者信息

  • 1. 甘肃中金黄金矿业有限责任公司,甘肃 陇南 742400
  • 2. 中国地质大学(北京)地质过程与矿产资源国家重点实验室,北京 100083||中国地质大学(北京)地球科学与资源学院,北京 100083
  • 3. 中国黄金集团有限公司,北京 100011
  • 折叠

摘要

Abstract

The newly identified jamesonite in the Dadiangou gold deposit,Liangdang County,Gansu Prov-ince,is closely associated with stibnite,galena,pyrite,and quartz.Detailed mineralogical,electron probe microanalysis(EPMA)and X-Ray Powder Diffraction(XRPD)reveal that its chemical composition(average formula Fe1.02Pb4.51Sb5.92S14.00)and crystal structure(monoclinic system,a=1.5383 nm,b=1.8716 nm,c=0.3937 nm)are in good agreement with theoretical values.This study not only identifies the mineral itself but,more importantly,we use its specific occurrence and composition as key geochemical indicators.The formation of jamesonite clearly indicates the injection of magma-derived fluids with high sulfur fugacity and enriched in Pb and Sb during the late stage of gold mineralization.This discovery provides robust mineralogical evidence for the involvement of magmatic-hydrothermal processes in the formation of the deposit under the shallow,variable geological conditions,thereby deepening the understanding of the mineralization mechanisms in this region.

关键词

脆硫锑铅矿/矿物学特征/成因意义/大店沟金矿/甘肃

Key words

jamesonite/mineralogy/genetic significance/Dadiangou Gold Deposit/Gansu

分类

天文与地球科学

引用本文复制引用

樊荣,司明扬,刘家军,张斌,曹瑞荣,来召,艾忠林,于谦,杜佰松..甘肃大店沟金矿床中脆硫锑铅矿的发现与成矿启示[J].现代地质,2026,40(4):1023-1033,11.

基金项目

中国黄金集团地质有限公司项目"西秦岭地区李子园—大店沟一带金矿成矿规律与找矿预测研究"(2024-09) (2024-09)

国家自然科学重点基金项目"秦岭造山带金矿床中低熔点亲铜元素对金的超常富集作用与成矿机制"(42430813). (42430813)

现代地质

1000-8527

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