微细浸染型金矿床的盆地流体成因模式  

Basin fluid genetic model of micro-disseminated gold deposit

作　　者：李明涛[1] 梁敬[1] 

机构地区：[1]吉林省有色金属地质勘查局六0七队,吉林吉丰132105

出　　处：《有色金属文摘》2015年第3期22-22,24,共2页Nonferrous Metals Abstract

摘　　要：盆地地形的沉积岩体系有着更为微观的物质促进金矿的发育和形成,流体则是其中一个非常关键的促成体。本文以沉积盆地中微细浸染型金矿床作为例子,来说明盆地流体的特征及成因。In the topography of the basin sedimentary system, there are more micro material to promote the development and formation of a gold mine,and the fluid is one of the very important materials. In this paper the author uses the micro disseminat ed gold deposits in sedimentary basin as an example, to illustrate the characteristics and genesis of the basin fluid.

关 键 词：沉积盆地 脱水排水 水岩反应 

分 类 号：TD95[矿业工程—选矿]