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The Bingham Canyon Porphyry Cu-Mo-Au Deposit. III. Zoned Copper-Gold Ore Deposition by Magmatic Vapor Expansion

机译:宾厄姆峡谷斑岩铜钼金矿床。三,岩浆蒸汽扩展对铜金矿的分区沉积

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摘要

Fluid inclusion microthermometry and laser-ablation ICPMS microanalysis are combined with geological and textural observations to reconstruct the spatial and temporal evolution of magmatic fluids that formed the subvolcanic porphyry Cu-Au(-Mo) ore deposit at Bingham Canyon, Utah. The Bingham Canyon orebody is exposed over ~1.6 km vertically and has the shape of an inverted cup with distinct metal zoning.
机译:流体包裹体热计量学和激光烧蚀ICPMS微观分析 与地质和构造观测相结合,重建 形成 的岩浆的时空演化。 Utah的Bingham Canyon的次火山岩斑岩Cu-Au(-Mo)矿床。宾厄姆峡谷矿体垂直暴露于〜1.6 km处 ,呈倒杯状,具有明显的金属分区。

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  • 来源
    《Economic Geology》 |2010年第1期|91-118|共28页
  • 作者单位

    ETH Zurich, Department of Earth Sciences, Clausiusstrasse 25, 8092 Zurich, Switzerland;

    ETH Zurich, Department of Earth Sciences, Clausiusstrasse 25, 8092 Zurich, Switzerland;

    Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305;

    ETH Zurich, Department of Earth Sciences, Clausiusstrasse 25, 8092 Zurich, Switzerland;

    ETH Zurich, Department of Earth Sciences, Clausiusstrasse 25, 8092 Zurich, Switzerland;

    ETH Zurich, Department of Earth Sciences, Clausiusstrasse 25, 8092 Zurich, Switzerland, and Faculty of Mathematics and Natural Sciences, University of Zurich;

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