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四川甘孜-理塘断裂带中段阿加隆洼金矿围岩蚀变特征及与金矿化关系
引用本文:肖军,孙传敏,刘严松,马子宁,杨弘忠,周庆磊,孙遥.四川甘孜-理塘断裂带中段阿加隆洼金矿围岩蚀变特征及与金矿化关系[J].地质与勘探,2008,44(6):8-12.
作者姓名:肖军  孙传敏  刘严松  马子宁  杨弘忠  周庆磊  孙遥
作者单位:1. 成都理工大学地球科学学院,成都,610051
2. 四川省地质矿产勘查开发局应用地球物理研究所,西昌,615000
3. 重庆市地质勘查局川东南地质队,重庆,400038
基金项目:四川省杰出青年学科带头人培养计划项目(编号:06ZQ026-014)资助
摘    要:阿加隆洼金矿是近年来在甘孜-理塘断裂带发现的一个中型低温热液型金矿床.区内围岩蚀变发育广泛,具多期次,蚀变类型主要有硅化、碳酸盐化、黄铁矿化、毒砂化、绿泥石化等.文章在介绍阿加隆洼金矿床区域地质背景、矿床特征、矿体地质特征的基础上,着重对矿床的围岩蚀变特征进行了较为深入地论述,并分析了该矿床的成矿地质条件.认为矿化蚀变岩带与金矿化关系密切,尤其与硅化、碳酸岩化、黄铁矿化最为密切,并且含矿热液在迁移过程中,与围岩发生的流体 - 岩石反应,造成金的沉淀、富集,最终形成金矿床.

关 键 词:围岩蚀变  金矿化  阿加隆洼金矿  矿床成因

WALLROCK ALTERATION AND RELATION WITH GOLD MINERALIZATION OF AJIALONGWA GOLD DEPOSIT IN THE CENTRAL GANZI-LITANG FAULT ZONE,SICHUAN
XIAO Jun,SUN Chuan-min,LIU Yan-song,MA Zi-ning,YANG Hong-zhong,ZHOU Qing-lei,Sun Yao.WALLROCK ALTERATION AND RELATION WITH GOLD MINERALIZATION OF AJIALONGWA GOLD DEPOSIT IN THE CENTRAL GANZI-LITANG FAULT ZONE,SICHUAN[J].Geology and Prospecting,2008,44(6):8-12.
Authors:XIAO Jun  SUN Chuan-min  LIU Yan-song  MA Zi-ning  YANG Hong-zhong  ZHOU Qing-lei  Sun Yao
Institution:1.College of Earth Science;Chengdu University of Technology;Chengdu 610051;2.Institute of Applied Geophysics;Sichuan Bureau of Geological Exploration and Exploitation of Mineral Resources;Xichang 615000;3.Geological Team of Southeastern Sichuan;Chongqing Bureau of Geological Exploration and Exploitation of Mineral Resources;Chongqing 400038
Abstract:Ajialongwa gold deposit,discovered in the Ganzi-Litang fault zone,is a middle scale epithermal gold deposits.Wallrock alterations are distributed widely in the area.Wallrock alterations include silicification,pyritization,carbonation and arsenopyritezation,and chloritization.Based on regional geological setting,deposit characteristics,geologic features of deposit,wallrock alterations and ore-forming geological conditions are summed up.It is considered that alterations zones,particularly silicification,carbo...
Keywords:wallrock alteration  Au mineralization  Ajialongwa gold deposit  ore genesis  
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