| 青海赛什塘─日龙沟矿田岩浆岩与成矿的关系探讨 |
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| 引用本文： | 田生玉.青海赛什塘─日龙沟矿田岩浆岩与成矿的关系探讨[J].岩土工程界,1999(6). |
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| 作者姓名： | 田生玉 |
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| 作者单位： | 青海有色地质勘查局七队!平安810600 |
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| 摘 要： | 赛什塘─日龙沟矿田受南秦岭印支地槽西端海南三叠纪沉降盆地西缘的同生断裂控制，矿床（ 点） 具“三位一体”特征，它们无论在空间上、时间上还是成因上与钙碱性岩浆岩存在着密切的内在联系，可能属于斑岩型矿床组合
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| 关 键 词： | 青海 赛什塘─日龙沟矿田 石英闪长杂岩体 |
RELATIONS BETWEEN MAGMATIC ROCKS AND METALLIZATION OF THE SAISHITANG-RILONGGOU ORE FIELD IN QINGHAI |
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| Tian Shengyu.RELATIONS BETWEEN MAGMATIC ROCKS AND METALLIZATION OF THE SAISHITANG-RILONGGOU ORE FIELD IN QINGHAI[J].Geotechnical Engineering World,1999(6). |
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| Authors: | Tian Shengyu |
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| Abstract: | The Saishitang-Rilonggou ore field in Qinghai is controlled by the contemporaneous faults on the western margin of Hainan Triassic basin, west of Qinling Indosinian geosyncline. Featuring trinity, it has close relation to calcic-alkalic magmatism in space, time and origin. It may be porphyry ore deposit. |
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| Keywords: | Qinghai Saishitang-Rilonggou quartz diorite complex porphyry isotope |
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