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