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地球学报  2004 

医巫闾山变质核杂岩中金矿的稳定同位素特征

Keywords: 变质核杂岩,稳定同位素,医巫闾山,金矿

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Abstract:

医巫闾山变质核杂岩中金矿及相关岩石的氢、氧、铅、硅、碳、硫稳定同位素测试结果为：成矿流体泐为-97‰～-72‰，δ^18O为0．3‰～3．8‰，在δ^18O-δD分布图上，位于变质水、岩浆水与当地雨水之间；其他稳定同位素数据及综合资料均说明，以排山楼金矿为代表的该区金矿成矿具有长期性、复杂性和多源性；医巫闾山变质核杂岩构造系统对区内金矿有一定控制作用。

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