| 赛什腾山地区构造地质特征及金矿化 |
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| 引用本文： | 赵子基,陈树旺,国家辉.赛什腾山地区构造地质特征及金矿化[J].地质与资源,1997,6(3):199-203. |
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| 作者姓名： | 赵子基 陈树旺 国家辉 |
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| 作者单位： | 1. 青海地矿局第一地质大队;2. 沈阳地质矿产研究所 |
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| 摘 要： | 赛什腾山地区构造活动比较强烈,NW向的褶皱构造与断裂构造构成了本地区的构造格架,控制了区域地层、岩浆岩以及金矿床(点)的产出.NW向主体构造是区域性矿液活动的通道.其次级构造为金矿化提供了就位空间.
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| 关 键 词： | 构造 金矿化 赛什腾山 青海省 |
| 收稿时间： | 1997-06-01 |
STRUCTURAL GEOLOGY AND GOLD MINERALIZATION OF SAISHITENG MOUNTAIN AREA |
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| Zhao Ziji,Chen Shuwang,Guo Jiahui.STRUCTURAL GEOLOGY AND GOLD MINERALIZATION OF SAISHITENG MOUNTAIN AREA[J].Geology and Resources,1997,6(3):199-203. |
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| Authors: | Zhao Ziji Chen Shuwang Guo Jiahui |
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| Institution: | 1. No. 1 Geological Team, Bureau of Geology and Mineral Resources, Qinghai Province;2. Shenyang Institute of Geology and Mineral Resources |
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| Abstract: | The structural activity in Saishiteng Mt.area is relatively strong.NW trending folds and faults made up the structural framwork of the area,and controlled the distribution of strata,magmatite and gold deposits(spots).The major structure running NW served as the channel of ore solusion.Its secondary structure supplied the emplacing space for gold mineralization. |
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| Keywords: | structure gold mineralization Saishiteng Mountain Qinghai Province |
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