| 高岭土矿成因分类的氢氧同位素证据 |
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| 引用本文： | 赵连才,林蓉南. 高岭土矿成因分类的氢氧同位素证据[J]. 资源调查与环境, 1992, 0(3) |
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| 作者姓名： | 赵连才 林蓉南 |
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| 作者单位： | 南京地质矿产研究所(赵连才)，南京地质矿产研究所(林蓉南) |
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| 摘 要： | 本文论述了氢、氧同位素作为高岭土矿成因类型地球化学指标的意义.根据氢、氧同位素数据,我国浙闽沿海地区高岭土矿床主要可分为热液蚀变型和风化作用型两大类.其成矿溶液以大气降水为主.
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| 关 键 词： | 高岭土矿床 氢、氧不同位素 成因类型 |
THE EVIDENCE OF HYDROGEN AND OXYSEN ISETOPE FOR GENETIC TYPE OF KAOLINE DEPOSITS |
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| Zhao Liacai Lin Rongnan. THE EVIDENCE OF HYDROGEN AND OXYSEN ISETOPE FOR GENETIC TYPE OF KAOLINE DEPOSITS[J]. Resources Survey & Environment, 1992, 0(3) |
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| Authors: | Zhao Liacai Lin Rongnan |
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| Abstract: | This paper discusses significance of stable hydrogen and oxygen isotopic geochcmical sign for type of kaoline deposits origin. Based on data of hydrogen and exygen isotope, kaoline deposits in coastal Zhejiang and Fugian, China, can mainly be classified into two types of hydrothermal alteration and weathering. Meteoric water is main compoment in the ore-forming fluids. |
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| Keywords: | Koaline deposit hydrogen and oxygen isotope genetic type. |
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