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首页> 外文期刊>Economic geology and the bulletin of the Society of Economic Geologists >Petrogenesis and Geodynamic Evolution of the Paleoproterozoic (similar to 1878 Ma) Trout Lake Volcanogenic Massive Sulfide Deposit, Flin Flon, Manitoba, Canada
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Petrogenesis and Geodynamic Evolution of the Paleoproterozoic (similar to 1878 Ma) Trout Lake Volcanogenic Massive Sulfide Deposit, Flin Flon, Manitoba, Canada

机译:加拿大马尼托巴省Flin Flon的古元古代(类似于1878 Ma)鳟鱼湖火山成块硫化物矿床的岩石成因和地球动力学演化

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摘要

The Trout Lake deposit (1878 +/- 1 Ma) is a rhyolite-hosted, bimodal-mafic, volcanogenic massive sulfide (VMS) deposit. It is one of the largest VMS deposits in the Flin Flon mining district, containing 21.8 Mt of Cu-Zn rich ore. The deposit underwent greenschist facies metamorphism and polyphase synvolcanic to postvolcanic hydrothermal alteration.
机译:鳟鱼湖矿床(1878 +/- 1 Ma)是流纹岩质,双峰基性,火山成岩的块状硫化物(VMS)矿床。它是Flin Flon矿区最大的VMS矿床之一,含有21.8 Mt的富含铜锌的矿石。该矿床经历了绿片岩相变质作用和多相同火山作用到火山后热液蚀变。

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