四川康定县磨玉台子金矿地质特征及找矿标志  

The Geological Feature and Prospecting Criteria of Moyutaizi Au Deposit in Kangding County,Sichuan Province

作　　者：邓小文[1] 刘磊[1] 李健[1] 吉树帮 马润轩 

机构地区：[1]成都理工大学地球科学学院,四川成都610059

出　　处：《四川有色金属》2015年第1期47-51,共5页Sichuan Nonferrous Metals

摘　　要：墨玉台子金矿位于滨太平洋成矿域上扬子成矿省康滇隆起成矿带康定孔玉-泸定Au成矿远景区内,是产于脆-韧性剪切带中典型的热液成因石英脉型金矿床。本文介绍了墨玉台子金矿产出的区域地质背景和矿区地质概况,详细总结了矿区内矿体特征、矿石特征以及围岩蚀变类型,并系统分析和归纳了各类找矿标志。Moyutaizi AU deposit belongs to the circum-pacific metallogenic domain Yangtze metallogenic province Kangdian uplift zone Kongyu-Luding Au metallogenic prospective areas, which is originated from brittle to ductile shear zone in the typical hydrothermal genesis of quartz vein type gold deposit. This paper introduces the general situation of the regional geological background and the mining area geological mining output, summarizes in detail the ore body characteristics, ore characteristics and wall rock alteration type, analysis and summarizes the various prospecting marks system.

关 键 词：金矿 石英脉型 地质特征 找矿标志 

分 类 号：P618[天文地球—矿床学]