| 吉林省二道甸子金矿床同位素地质学及矿床成因探讨 |
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| 引用本文： | 张文启 吴尚全. 吉林省二道甸子金矿床同位素地质学及矿床成因探讨[J]. 吉林地质, 1996, 15(2): 31-35 |
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| 作者姓名： | 张文启 吴尚全 |
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| 作者单位： | 吉林有色地质勘查局，武警黄金部队廊坊研究所 |
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| 摘 要： | 通过对二道甸子金矿床的硫、氢氧及铅同位素地质学研究，认为其成矿物质来源于周围地层，而成矿热液是以岩浆水为主的混合水，矿床成因属于岩浆活化型金矿。
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| 关 键 词： | 金矿床 同位素地质学 矿床成因论 |
ISOTOPE GEOLOGY OF THE ERDAODIANZI GOLD DEPOSIT IN JILIN PROVINCE AND ITS ORE GENESIS |
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| Zhang Wenqi. ISOTOPE GEOLOGY OF THE ERDAODIANZI GOLD DEPOSIT IN JILIN PROVINCE AND ITS ORE GENESIS[J]. Jilin Geology, 1996, 15(2): 31-35 |
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| Authors: | Zhang Wenqi |
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| Abstract: | By researching the O,S and Ph isotope geology of the Erdaodianzi gold ore deposit,it is indicated that the ore material was derved from the host rocks and the mineralizing fluid is a mixture dominated by magmatic water.The origin of ore deposit belongs to magmatic activation type. |
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| Keywords: | Erdaodianzi gold deposit Isotope geology Source of ore |
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