| 水晶屯金矿床稳定同位素地球化学研究 |
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| 引用本文： | 石森,杨廷栋.水晶屯金矿床稳定同位素地球化学研究[J].地质与资源,1997,6(1):38-46. |
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| 作者姓名： | 石森 杨廷栋 |
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| 作者单位： | 1. 地质矿产部地质调查局;2. 中国地质大学资源经济学院, 武汉 |
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| 基金项目： | 中国地质大学（武汉）与第一冶金地质勘查局合作项目 |
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| 摘 要： | 通过对水晶屯金矿床与区域上典型金矿床的硫、铅、氢、氧等稳定同位素的对比研究,阐明本区金矿成矿物质主要来源于太古宇崇礼杂岩,太古宙区域变质作用仅形成金的初步富集,印支-燕山早期的构造岩浆活动促成石英脉主体形成,燕山期继承性构造岩浆活动对先成脉体的叠加改造作用是成矿的重要因素,成矿流体来源于岩浆水.本矿床为具有层控性质的岩浆热液型矿床.
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| 关 键 词： | 水晶屯金矿 硫铅氢氧同位素 成矿作用 河北省 |
| 收稿时间： | 1996-10-03 |
SULFUR,LEAD,HYDROGEN AND OXYGEN ISOTOPIC GEOCHEMISTRY OF SHUIJINGTUN GOLD DEPOSIT IN HEBEI PROVINCE |
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| Shi Sen,Yang Tingdong.SULFUR,LEAD,HYDROGEN AND OXYGEN ISOTOPIC GEOCHEMISTRY OF SHUIJINGTUN GOLD DEPOSIT IN HEBEI PROVINCE[J].Geology and Resources,1997,6(1):38-46. |
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| Authors: | Shi Sen Yang Tingdong |
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| Institution: | 1. Bureau of Geological Survey, MGMR;2. China University of Geosciences, Wuhan |
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| Abstract: | By comparing Shuijingtun gold deposit with typical gold deposits in the same region on S Pb H O isotopic geochemistry,the authors conclude that metallogenetic material was derived mainly from Shuijingtun structural stratigraphic unit Archeozoic regional metamophism only resulted in initial enrichment of gold. Structural magmatic activity in Indo Chinese early Yanshan epoch helped to bring about the main body of quartz veins The inherited structural magmatic activity in Yanshan epoch was the main factor of gold mineralization Mineralizing fluid was mainly originated from magmatic water It's defined that Shuijingtun gold deposit is of stratabound magmatic hydrothermal type Its metallogenic modle is established |
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| Keywords: | Shuijingtun gold deposit S Pb H O isotopo mineralization Hebei Province |
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