首页> 外文期刊>Economic geology and the bulletin of the Society of Economic Geologists >Geology and District-Scale Setting of Tilted Alkalic Porphyry Cu-Au Mineralization at the Lorraine Deposit, British Columbia
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Geology and District-Scale Setting of Tilted Alkalic Porphyry Cu-Au Mineralization at the Lorraine Deposit, British Columbia

机译:不列颠哥伦比亚洛林矿床的倾斜碱性斑岩铜金矿化的地质学和区域尺度背景

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摘要

Lorraine is a copper-gold porphyry deposit (6.4 Mt indicated resource at 0.61% copper and 0.23 g/t gold, and 28.8 Mt inferred resource at 0.45% copper and 0.19 g/t gold) in north-central British Columbia-one of the youngest known alkalic porphyry deposits within the Triassic-Jurassic Quesnel arc. The deposit is hosted by the Early Jurassic Duckling Creek Syenite Complex, an alkalic multiphase intrusive dike complex of pyroxenite, syenite, and monzonite composition. The southern part of the complex hosts numerous copper-gold porphyry prospects in addition to Lorraine; together, they constitute the Duckling Creek district.
机译:Lorraine是不列颠哥伦比亚省中北部的铜金斑岩矿床(6.4 Mt的指示资源量为0.61%铜和0.23 g / t黄金,28.8 Mt的推测资源量为0.45%的铜和0.19 g / t黄金)在不列颠哥伦比亚省中北部。三叠纪-侏罗纪康奈尔弧内最年轻的已知碱性斑岩矿床。该矿床由早侏罗世小鸭溪Senenite矿床托管,这是一种由辉石矿,正长岩和Monzonite组成的碱性多相侵入式堤防综合体。除洛林市外,该综合体的南部还拥有许多铜金斑岩矿床。它们共同构成了Duckling Creek地区。

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