The relative effects of pressure, temperature and oxygen fugacity on the solubility of sulfide in mafic magmas

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Authors

Mavrogenes, John
O'Neill, Hugh

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Pergamon-Elsevier Ltd

Abstract

The sulfur contents at sulfide saturation (SCSS) of a basaltic and a picritic melt have been measured experimentally as a function of pressure and temperature from 5 to 90 kb and 1400-1800°C, using piston-cylinder and multi-anvil solid media pressure dev

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Citation

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Geochimica et Cosmochimica Acta

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Restricted until

2037-12-31