老挝爬奔金矿金矿化及其围岩蚀变过程元素迁移
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  • 英文篇名:Elements migration of gold mineralizatiom and wall-rock alteratiom process of the Phabon gold deposit in Laos
  • 作者:王杰亭 ; 谢建平 ; 卢邦飞 ; 刘争 ; 陈京玉 ; 康维刚 ; 张荣
  • 英文作者:WANG Jie-ting;XIEJian-ping;LU Bang-fei;LIU Zheng;CHEN Jing-yu;KANG Wei-gang;ZHANG Rong;Tianjin Huakan Laos Mining Company Ltd;Inner Mongolia Geological Engineering Co., Ltd.;Tianjin Huakan Mining Investment Ltd;
  • 关键词:水岩反应 ; 矿化蚀变 ; 围岩 ; 岩浆热液 ; W异常
  • 英文关键词:water-rock reaction;;mineralizatiom and wall-rock alteratiom;;wall-rock;;magama;;W anomaly
  • 中文刊名:QHWJ
  • 英文刊名:Geological Survey and Research
  • 机构:天津华勘老挝矿业有限公司;内蒙古地质工程有限责任公司;天津华勘矿业投资有限公司;
  • 出版日期:2018-06-15
  • 出版单位:地质调查与研究
  • 年:2018
  • 期:v.41;No.162
  • 基金:国外矿产资源风险勘查专项基金项目“老挝琅勃拉邦省巴乌县金铜多金属矿普查和详查(201211B00200006)”
  • 语种:中文;
  • 页:QHWJ201802005
  • 页数:6
  • CN:02
  • ISSN:12-1353/P
  • 分类号:30-34+55
摘要
根据水岩反应理论,通过对矿化蚀变岩与围岩的对比分析,对爬奔金矿围岩在矿化蚀变过程中的元素迁移规律进行了分析研究,结果表明在金矿化热液蚀变过程中,不同元素带入带出程度不同,具有一定的迁移规律,主要带入元素为Au、Hg、As、W,元素W的带入说明含矿热液可能与深部岩浆有关,地球化学W异常为后期找矿提供了新的指示性线索。
        According to the water-rock reaction theory, through the comprative analysis of surrouding rocks and altered rocks, as well as the elements migrations study covers the phyllite process of mineralizatiom and alteration in the Phabon gold deposit.It is shown that various elements are carried in and out at different degrees in the process of gold mineralization and alteration,the element migration is obvious.The main elements is Au、Hg、As、W which have been brought into wall-rock. Element W maybe illustrate that hydrothermal fluids may be associated with deep magma.we were used to ignore W anomaly. After this study, we know that anomaly W is closely related to the ore-bearing hydrothermal fluid, which provides new indicator clues for the later geological exploration.
引文
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