| 华南地洼阶段低温地球化学作用与硅化岩-交代石英岩 |
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| 引用本文： | 刘汉元,刘立钧.华南地洼阶段低温地球化学作用与硅化岩-交代石英岩[J].中南大学学报(自然科学版),1991(3). |
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| 作者姓名： | 刘汉元 刘立钧 |
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| 作者单位： | 中南工业大学，中南地勘局230研究所 |
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| 摘 要： | 本文以较全面的资料数据,论述了两种不同类型硅化岩-交代石英岩的地球化学特征、交代机制、成因及与矿的关系。
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| 关 键 词： | 地洼 低温交代 硅化岩—交代石英岩 |
LOW TEMPERATURE GEOCHEMICAL PROCESS OF DIWA STAGE AND SILICIFIED ROCK-METASOMATIC QUARTZITE, SOUTHERN CHINA |
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| Liu Hanyuan,Liu Lijun.LOW TEMPERATURE GEOCHEMICAL PROCESS OF DIWA STAGE AND SILICIFIED ROCK-METASOMATIC QUARTZITE, SOUTHERN CHINA[J].Journal of Central South University:Science and Technology,1991(3). |
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| Authors: | Liu Hanyuan Liu Lijun |
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| Institution: | Liu Hanyuan,Liu Lijun Department of Geology,Central-South University of Technology Research Institute No. 230,Central Southern Bureau China National Nuclear Corporation |
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| Abstract: | Two types of silicified rock-metasomatic quatrzites which are different in fabric, occurrence, shapeand mineralization are presented in this paper. Based on sufficient data, the authors described their geo-chemical characteristics, metasomatism mechanism and geneses etc. |
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| Keywords: | diwa low temperature metasomatism silicified rock-metasomatic quartzite |
| 本文献已被 CNKI 等数据库收录！ |
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