| 红花沟金矿床地质特征及矿床成因研究 |
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| 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. |
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| 作者姓名： | 张百胜 |
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| 作者单位： | 内蒙古有色地质勘查局108队, |
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| 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。
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| 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年11月27 |
STUDY ON GEOLOGICAL CHARACTERS OF HONGHUAGOU GOLD DEPOSIT AND THE GENESIS OF ITS DEPOSITION |
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| 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. |
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| Authors: | ZHANG Bai sheng |
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| 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. |
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| Keywords: | Geological character of deposit Mineral inclusion Deposit genesis Indicator for exploration Honghuagou gold deposit |
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