关于黔西南高砷煤与卡林型金矿的思考  

Thinking about in high arsenic coal and Carlin type gold deposits

作　　者：聂荣[1,2] 蒙明华 

机构地区：[1]贵州省地矿局105地质大队,贵州贵阳550018 [2]贵州大学资源与环境工程学院,贵州贵阳550025

出　　处：《世界有色金属》2017年第14期185-186,共2页World Nonferrous Metals

摘　　要：黔西南地区是我国卡林型(微细浸染型)金矿的主要分布区,也是高砷煤的主要产区。近年来,众多学者对该地区卡林型金矿地质特征、成矿背景、成矿规律及高砷煤的特征、成因作了大量研究,成果表明该地区高砷煤的形成与卡林型金矿的成矿属于同一系统。鉴于这种特殊联系,该地区的高砷煤会是"高金煤"吗?笔者将在本文就此展开讨论。The southwestern Guizhou area is Carlin type（disseminated） the main distribution area of gold, is the main producing areas of high arsenic coal. In recent years, many scholars have made a lot of research on the geological characteristics of the region, the Carlin type gold mineralization background, metallogenic regularity and characteristics, the results showed that the high arsenic coal formation, mineralization in the area with high arsenic coal formation of Carlin type gold deposits belong to the same system. In view of this special relationship, the area of high arsenic coal will be ＂high coal＂ ？ The author will discuss this at this point.

关 键 词：高砷煤 卡林型金矿 “高金煤” 黔西南 

分 类 号：P618.51[天文地球—矿床学]