ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
义敦弧北段首次发现大型中硫化型浅成低温热液富金银铅锌铜矿床
  
关键词:Xia’nanggou  Au-Ag-Pb-Zn-Cu deposit  intermediate-sulfidation  epithermal deposit  phreatomagmatic breccia  Yidun Arc
基金项目:本文由杭州越昌科技有限公司“四川白玉县夏囊沟铅锌矿控矿因素及找矿潜力研究”项目(编号: AH2025-0483)和四川省科技厅“川西可尔因锂矿田矿物地球化学-高光谱勘查建模”项目(编号: 2026NSFSC1144)联合资助。
作者单位E-mail
冉凤琴 成都理工大学地球与行星科学学院 422713652@qq.com 
柳维君 四川省金属地质调查研究所 29920529@qq.com 
张博 四川省金属地质调查研究所  
彭勃 成都理工大学地球与行星科学学院 p.engbo@163.com 
王国富 杭州越昌科技有限公司  
邓辉 成都理工大学地球与行星科学学院  
杨洪伟 四川省金属地质调查研究所  
田欢欢 四川省金属地质调查研究所  
杨彦宏 杭州越昌科技有限公司  
赵媛 成都理工大学地球与行星科学学院  
代涌坤 成都理工大学地球与行星科学学院  
王思睿 成都理工大学地球与行星科学学院  
韩警锐 成都理工大学地球与行星科学学院  
孙崇波 四川省金属地质调查研究所  
高学震 四川省金属地质调查研究所  
刘严松 成都理工大学地球与行星科学学院  
鲁军 成都理工大学地球与行星科学学院  
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摘要:
The First Discovery of a Large Intermediate-sulfidation Epithermal Au-Ag-Pb-Zn-Cu Deposit in the Northern Segment of the Yidun Arc
      The Xia’nanggou deposit is a newly discovered Au-Ag-Pb-Zn-Cu mineralization system in the northern segment of the Yidun Arc (SW China). Based on integrated field mapping, drill core logging, petrographic observations, and shortwave infrared (SWIR) spectral analysis, we documented its geological characteristics, ore control, and genetic type. Orebodies occur as steep, tabular to pipe-like shoots hosted by Upper Triassic Mengge Formation tuffs and are jointly controlled by NW-trending faults and a concealed phreatomagmatic breccia pipe. The ore textures include veinlet-stockwork-disseminated, brecciated, and massive styles. The principal sulfide assemblages are sphalerite, galena, chalcopyrite, tetrahedrite, and tennantite. The alteration is well-zoned, with an inner silicifica-tion-sericitization core grading outward to a sericite-argillic zone and a distal propylitic halo, and the dominant al-teration minerals are quartz-carbonate-muscovite-illite. A vertical metal zonation was observed from Pb-Zn in the shallow levels to Cu-Pb-Zn at intermediate depths and Cu (with elevated Au and Ag) at depth. Collectively, these features indicate an intermediate sulfidation epithermal system. This discovery expands the recognized deposit spectrum of the northern Yidun Arc and suggests a potential for porphyry-epithermal metallogenic systems within Late Triassic volcanic sequences.
RAN Fengqin,LIU Weijun,ZHANG Bo,PENG Bo,WANG Guofu,DENG Hui,YANG Hongwei,TIAN Huanhuan,YANG Yanhong,ZHAO Yuan,DAI Yongkun,WANG Sirui,HAN Jingrui,SUN Chongbo,GAO Xuezhen,LIU Yansong,LU Jun.2026.The First Discovery of a Large Intermediate-sulfidation Epithermal Au-Ag-Pb-Zn-Cu Deposit in the Northern Segment of the Yidun Arc[J].Acta Geoscientica Sinica,47(2):235-248.
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