| 四川底苏、大梁子铅锌矿床中方铅矿和黄铁矿地球化学标型特征 |
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| 引用本文： | 朱赖民,袁海华.四川底苏、大梁子铅锌矿床中方铅矿和黄铁矿地球化学标型特征[J].四川地质学报,1995(3). |
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| 作者姓名： | 朱赖民 袁海华 |
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| 作者单位： | 成都理工学院 |
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| 基金项目： | 四川省地矿局“八五”科研项目 |
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| 摘 要： | 通过底苏、大梁子铅锌矿床中的方铅矿和黄铁矿的化学成分、同位素地球化学、爆烈温度等方面研究，作者认为两矿床属沉积改造层控矿床，成矿温度为中低温．
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| 关 键 词： | 方铅矿，黄铁矿，地球化学标型特征，底苏，大梁子 |
TYPOMORPHIC CHARACTERISTICS OF GEOCHEMISTRY OF GALENA AND PYRITE FROM DISU AND DALIANGZI Pb-Zn DEPOSITS,SICHUAN |
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| Zhu Laimin and Yuan Haihua.TYPOMORPHIC CHARACTERISTICS OF GEOCHEMISTRY OF GALENA AND PYRITE FROM DISU AND DALIANGZI Pb-Zn DEPOSITS,SICHUAN[J].Acta Geologica Sichuan,1995(3). |
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| Authors: | Zhu Laimin and Yuan Haihua |
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| Institution: | Chengdu Institute of Technology |
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| Abstract: | Based on the research on chemical composition,isotope geochemistry and decrepitation of galena and pyrite from Disu and Daliangzi Pb-Zn deposits,the authors regard them as sedimentary-reformation type stratabound deposits with low or medium mineralization temperature. |
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| Keywords: | galena pyrite typomorphic characteristic of geochemistry Disu Daliangzi |
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