| 铅同位素地球化学示踪进展 |
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| 引用本文： | 何琼,李向阳.铅同位素地球化学示踪进展[J].地质找矿论丛,1998,13(3):79-82. |
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| 作者姓名： | 何琼 李向阳 |
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| 作者单位： | [1]中国地质大学研究生院 [2]中国地质大学地球化学研究所 |
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| 摘 要： | 本文论述了铅同位素示在地学中的最新应用和发展。由于它在示踪物质来源，圈定找矿靶区，判别构造环境等方面的优势，是当前最重要的地球化学示踪手段之一和同位素地球化学研究的热点。
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| 关 键 词： | 地球化学示踪 同位素地球化学 铅 |
| 收稿时间： | 1998/3/10 0:00:00 |
| 修稿时间： | 1998/4/8 0:00:00 |
DEVELOPMENT OF GEOLOGICAL TRACING OF LEAD ISOTOPES |
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| He Qiong and Li Xiangyang.DEVELOPMENT OF GEOLOGICAL TRACING OF LEAD ISOTOPES[J].Contributions to Geology and Mineral Resources Research,1998,13(3):79-82. |
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| Authors: | He Qiong and Li Xiangyang |
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| Institution: | Class 951, Graduate School, China University of Geosciences, Wuhan, 430074;Instittute of Geochemistry, China University of Geosciences, Wuhan, 430074 |
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| Abstract: | As an important geoloical tracing method,lead(Pb)isotopes have their unique advantages to be used in tracing the material origin,sorting the unknown mineral deposits,discriminating the tectonic background etc.The main application and present progress are discussed in details in this paper. |
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| Keywords: | Lead(Pb)isotope geochemical tracing Isotopic geochemistry |
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