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Research Collection Journal Article Hematite-breccia Hosted Iron Oxide Copper-Gold Deposits Require Magmatic Fluid Components Exposed to Atmospheric Oxidation: Evidence from Prominent Hill, Gawler Craton, South Australia Author(s): Schlegel, Tobias U.; Wagner, Thomas; Wälle, Markus; Heinrich, Christoph A. Publication Date: 2018-05-01 Permanent Link: https://doi.org/10.3929/ethz-b-000267650 Originally published in: Economic Geology 113(3), http://doi.org/10.5382/econgeo.2018.4564 Rights / License: In Copyright - Non-Commercial Use Permitted This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms of use. ETH Library This is the Green Open Access version of: Schlegel, T. U., Wagner, T., Wälle, M., and Heinrich, C. A., 2018. Hematite-breccia hosted iron oxide–copper–gold deposits require magmatic fluid components exposed to atmospheric oxidation: Evidence from Prominent Hill, Gawler craton, South Australia. Economic Geology, v. 113, p. 597-644. Original publication see: https://doi.org/10.5382/econgeo.2018.4564 Hematite-breccia hosted iron oxide–copper–gold deposits require magmatic fluid components exposed to atmospheric oxidation: Evidence from Prominent Hill, Gawler craton, South Australia Tobias U. Schlegel1,*, Thomas Wagner2, Markus Wälle1,# and Christoph A. Heinrich1,3 1Institute of Geochemistry and Petrology, ETH Zürich, 8092 Zürich, Switzerland 2Institute of Applied Mineralogy and Economic Geology, RWTH Aachen University, Germany 3Also at: Faculty of
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