| 陕西镇安丘岭微细浸染型金矿床同位素组成特征及成因意义 |
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| 引用本文： | 申萍.陕西镇安丘岭微细浸染型金矿床同位素组成特征及成因意义[J].地质找矿论丛,1996,11(4):27-34. |
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| 作者姓名： | 申萍 |
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| 作者单位： | 西安矿业学院地质系 |
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| 摘 要： | 本文通过硫、氢、氧、碳、铅同位素组成的研究，认为成矿溶液来自大气降水，成矿物质来自南羊山组和袁家沟组的不纯细碎屑岩－碳酸盐岩。在此基础上分析了成矿过程。
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| 关 键 词： | 同位素 组成特征 金矿床 浸染型矿床 |
| 收稿时间： | 1996/7/15 0:00:00 |
ISOTOPIC COMPOSITIONS IN THE QIULING MICRODISSEMINATED GOLD DEPOSIT, ZHEN'AN COUNTY, SHANXI PROVINCE, AND THEIR GENETIC IMPLICATIONS |
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| Shen Ping.ISOTOPIC COMPOSITIONS IN THE QIULING MICRODISSEMINATED GOLD DEPOSIT, ZHEN''AN COUNTY, SHANXI PROVINCE, AND THEIR GENETIC IMPLICATIONS[J].Contributions to Geology and Mineral Resources Research,1996,11(4):27-34. |
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| Authors: | Shen Ping |
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| Institution: | Department of Geology, Xi''an Mining Institute |
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| Abstract: | This paper presents S, H, O, C isotopic data obtained from Qiuling micro-fine disseminated gold deposit. H2O in.ore fluid is mainly from ancient meteoric water. Ore-forming materials are dominated by those derived from impure-fine clasitic carbonate rock of Nanyangshan Formation and Yuanjiagou Formation. Then ore-forming processes are analysed. |
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