| 我国金红石矿床成因类型及成矿区带 |
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| 引用本文： | 徐少康.我国金红石矿床成因类型及成矿区带[J].化工矿产地质,2001,23(1):11-18. |
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| 作者姓名： | 徐少康 |
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| 作者单位： | 化学矿产地质研究院 |
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| 摘 要： | 我国金红石矿床分为 10大成因类型 :高、超高压正变质型、中高压正变质类型、中低压正变质类型、中高压负变质类型、低压负变质类型、变质蚀变型、岩浆型、热液充填型、热液蚀变型及沉积型 ;前6种类型常为大型 ,是主要类型。有 5个成矿区带 :东秦岭成矿带、太行恒山成矿带、鲁东成矿区、湘东北成矿区及东南沿海成矿带 ,前两个是主要成矿带
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| 关 键 词： | 金红石矿床 成因类型 成矿区带 找矿方向 中国 |
| 修稿时间： | 2000年11月22 |
GENETIC TYPES OF MINERALIZING PROVINCES OF RUTILE DEPOSITS IN CHINA |
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| Xu Shaokang.GENETIC TYPES OF MINERALIZING PROVINCES OF RUTILE DEPOSITS IN CHINA[J].Geology of Chemical Minerals,2001,23(1):11-18. |
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| Authors: | Xu Shaokang |
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| Institution: | Geological Institute for Chemical Minerals |
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| Abstract: | Rutile deposits in China are grouped into ten genetic types including: super high-pressure ortho-metamorphic, medium-high-pressure ortho-metamorphic, medium- low-pressure ortho-metamorphic, medium-high-pressure para-metamorphic, low-pressure para-metamorphic, metamorphical altered, magmatic, hydrothermal infilled, hydrothermal altered and sedimentary. The first six types tend to form large-sized deposits, thus regarded as important genetic types. As for mineralizing provinces of rutile deposits, such five provinces have been located as East Qinling range, Taihangshan-Henshan mountain chain, East Shandong, Northeast Hunan and Southeast coastal areas. The first two provinces are of importance. |
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| Keywords: | rutile deposit genetic types mineralizing provinces ore-hunting direction China |
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