| 豫西熊耳山青岗坪金矿床特征及其稳定同位素研究 |
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| 引用本文： | 陈旺,崔亳,徐孟罗,郭时然.豫西熊耳山青岗坪金矿床特征及其稳定同位素研究[J].地质与资源,1996,5(3):213-217. |
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| 作者姓名： | 陈旺 崔亳 徐孟罗 郭时然 |
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| 作者单位： | 河南有色地勘局研究所 |
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| 摘 要： | 青岗坪金矿为缓倾式构造蚀变岩型金矿床,具产状干缓、矿体薄、品位高、延伸长的特点。成矿物质主要来源于花山花岗岩,是燕山期花岗岩浆活动的产物,具有大中型矿床成矿条件。
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| 关 键 词： | 豫西 青岗坪 金矿 缓倾式 稳定同位素 花岗岩 |
| 收稿时间： | 1996-02-10 |
THE FEATURE OF QINGGANGPING GOLD DEPOSIT AND STUDY ON THE STABIE ISOTOPE, XIONGERSHAN AREA,WESTERN HENAN PROVINCE |
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| Chen Wang,Cui Bo,Xu Mengluo,Guo Shiran.THE FEATURE OF QINGGANGPING GOLD DEPOSIT AND STUDY ON THE STABIE ISOTOPE, XIONGERSHAN AREA,WESTERN HENAN PROVINCE[J].Geology and Resources,1996,5(3):213-217. |
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| Authors: | Chen Wang Cui Bo Xu Mengluo Guo Shiran |
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| Institution: | Henan Institute of Nonferrous Metal Mineral Resources and Geology |
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| Abstract: | Qinggangping deposit is a low-angle altered fractural rock type gold deposit. It is low-angle, thin,high grade and long extending. The study on stable isotopes suggests the metallo-genic material derived from Huashan granite. As other gold deposits in Xiongershan area the deposit is formed by Yanshannian granite. There are metallogenic conditions for middle -large scale gold deposits. |
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| Keywords: | western Henan Qinggangping gold deposit low-angle type stable isotopes granit |
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