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The nature of iron oxide-copper-gold ore fluids: Fluid inclusion evidence from Norrbotten (Sweden) and the Cloncurry district (Australia)

机译:氧化铁 - 铜金矿流体的性质:来自Norrbotten(瑞典)和Cloncurry区(澳大利亚)的流体包含证据

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摘要

Fluid inclusions from two key iron oxide-copper-gold ore provinces (including data from mined deposits at Aitik and Pahtohavare in Norrbotten; and Ernest Henry, Mount Elliott, Osborne and Starra near Cloncurry) reveal distinctive features compared to other types of hydrothermal ore deposit. Many different types of fluid inclusions occur but the most common are mixed populations of a) liquid-rich carbonic (CO_2 +-
机译:来自两个关键氧化铁 - 铜金矿省的流体夹杂物(包括来自Norrbotten的Aitik和Pahtohavare的矿山沉积物的数据;与其他类型的热热矿床相比,奥纳姆斯亨利。许多不同类型的液体夹杂物发生,但最常见的是A)富含富含液体的碳化物(CO_2 + -

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