Fluids as primary carriers of sulphur and copper in magmatic assimilation

Experiments show that when magma heats black shale wall-rock, fluids form and mobilize S and Cu, which can then concentrate and form base metal deposits. The fluids also attach to sulphide droplets and cause them to float in the host silicate melt.

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Autores principales: Ville J. Virtanen, Jussi S. Heinonen, Ferenc Molnár, Max W. Schmidt, Felix Marxer, Pietari Skyttä, Nico Kueter, Karina Moslova
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/4d8592ebab8946f0a6623e2609b7c148
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Sumario:Experiments show that when magma heats black shale wall-rock, fluids form and mobilize S and Cu, which can then concentrate and form base metal deposits. The fluids also attach to sulphide droplets and cause them to float in the host silicate melt.