红花沟金矿床地质特征及矿床成因研究  

STUDY ON GEOLOGICAL CHARACTERS OF HONGHUAGOU GOLD DEPOSIT AND THE GENESIS OF ITS DEPOSITION

作　　者：张百胜 

机构地区：[1]内蒙古有色地质勘查局108队,内蒙古赤峰024000

出　　处：《矿产与地质》2001年第5期311-314,共4页Mineral Resources and Geology

摘　　要：通过矿物包裹体、硫同位素组成及氢、氧、碳同位素的研究 ,认为红花沟金矿床为燕山期中低温热液型黄铁矿 -石英脉型矿床 。Honghuagou gold deposit is considered to be lower temperature to hydrothemal type pyrite quartz vein type deposit with characteristics of multi period metamorphism according to the study of mineral inclusions, S isotope composition and H, O and C isotope.

关 键 词：矿床地质特征 矿物包裹体 矿床成因 找矿标志 金矿床 硫同位素 氢同位素 碳同位互 

分 类 号：P618.51[天文地球—矿床学]