Michael Mengason
University of Maryland, College Park, MD
Activity
2010
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THE SATURATION OF ANDESITIC MAGMA BY COPPER-IRON SULFIDE MINERALS AND LIQUIDS AS A FUNCTION OF OXYGEN FUGACITY, SULFUR FUGACITY, AND IRON TO COPPER RATIO OF THE MELT
T11 Vapors, Brines, Sulfides, and Mines: Understanding Metal Mobility in Magma-Hydrothermal Systems and Their Supergene SuccessorsSunday, 31 October 20108:00 AM - 12:00 PMRoom 601
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COPPER IN MAGMATIC EFFLUVIA
T11 Vapors, Brines, Sulfides, and Mines: Understanding Metal Mobility in Magma-Hydrothermal Systems and Their Supergene SuccessorsSunday, 31 October 20108:00 AM - 12:00 PMRoom 601