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Comparison of two end-member styles of epithermal Au-(Cu) deposits

机译:术术Au-(Cu)沉积物两端成员造型的比较

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摘要

Epitherma Au-(Cu) deposits occur largely in volcano-plutonic arcs (island arcs as well as continental arcs) associated with subduction zones, with ages similar to those of volcanism. These deposits form at shallow depth, <1 km, and are hosted mainly by volcanic rocks.
机译:IPITHERMA AU-(CU)沉积物主要发生在与俯冲区相关的火山 - 浮雕弧(岛弧和大陆弧),随着VOLCANISIS的年龄而言。这些沉积物在浅深度,<1公里处,主要由火山岩托管。

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