| 红花沟金矿床地质特征及矿床成因研究 |
| |
| 引用本文： | 张百胜. 红花沟金矿床地质特征及矿床成因研究[J]. 矿产与地质, 2001, 15(5): 311-314 |
| |
| 作者姓名： | 张百胜 |
| |
| 作者单位： | 内蒙古有色地质勘查局108队, |
| |
| 摘 要： | 通过矿物包裹体、硫同位素组成氢、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，矿床具有多期改造的特征。
|
| 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 |
| 文章编号： | 1001-5663(2001)02-0311-04 |
| 修稿时间： | 2000-11-27 |
STUDY ON GEOLOGICAL CHARACTERS OF HONGHUAGOU GOLD DEPOSIT AND THE GENESIS OF ITS DEPOSITION |
| |
| ZHANG Bai sheng. STUDY ON GEOLOGICAL CHARACTERS OF HONGHUAGOU GOLD DEPOSIT AND THE GENESIS OF ITS DEPOSITION[J]. Mineral Resources and Geology, 2001, 15(5): 311-314 |
| |
| Authors: | ZHANG Bai sheng |
| |
| Abstract: | 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. |
| |
| Keywords: | Geological character of deposit Mineral inclusion Deposit genesis Indicator for exploration Honghuagou gold deposit |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
