Formation of magmatic sulfide deposits in arcs by reduction of oxidized basalt

Andrew George Tomkins; Kyle Rebryna; Roberto Ferrez Weinberg; Bruce Franklin Schaefer

Formation of magmatic sulfide deposits in arcs by reduction of oxidized basalt

Andrew George Tomkins, Kyle Rebryna, Roberto Ferrez Weinberg, Bruce Franklin Schaefer

Research output: Chapter in Book/Report/Conference proceeding › Conference Paper › Research › peer-review

Abstract

A region of magma mingling and mixing, containing magmatic sulfide mineralization, within a magmatic arc cross section in Hokkaido, Japan, is examined to explore the consequences of chemical equilibration between mantle-derived arc basalts and crust-derived graphite-bearing tonalites. Reduction of oxidized arc basalt, driven by buffering with contaminant graphite, is shown to be a viable mechanism for causing sulfide oversaturation.

Original language	English
Title of host publication	Abstracts, 11th International Platinum Symposium, 21-24 June 2010, Sudbury, Ontario, Canada
Editors	G H Brown, P J Jugo, C M Lesher, J E Mungall
Place of Publication	Sudbury Canada
Publisher	Ontario Geological Survey
Pages	1 - 4
Number of pages	4
ISBN (Print)	9781443533140
Publication status	Published - 2010
Event	International Platinum Symposium - Sudbury Ontario Canada, Sudbury Canada Duration: 1 Jan 2010 → …

Conference

Conference	International Platinum Symposium
City	Sudbury Canada
Period	1/01/10 → …

Cite this

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title = "Formation of magmatic sulfide deposits in arcs by reduction of oxidized basalt",

abstract = "A region of magma mingling and mixing, containing magmatic sulfide mineralization, within a magmatic arc cross section in Hokkaido, Japan, is examined to explore the consequences of chemical equilibration between mantle-derived arc basalts and crust-derived graphite-bearing tonalites. Reduction of oxidized arc basalt, driven by buffering with contaminant graphite, is shown to be a viable mechanism for causing sulfide oversaturation.",

author = "Tomkins, {Andrew George} and Kyle Rebryna and Weinberg, {Roberto Ferrez} and Schaefer, {Bruce Franklin}",

year = "2010",

language = "English",

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editor = "Brown, {G H} and Jugo, {P J} and Lesher, {C M} and Mungall, {J E}",

booktitle = "Abstracts, 11th International Platinum Symposium, 21-24 June 2010, Sudbury, Ontario, Canada",

publisher = "Ontario Geological Survey",

note = "International Platinum Symposium ; Conference date: 01-01-2010",

}

Tomkins, AG, Rebryna, K, Weinberg, RF & Schaefer, BF 2010, Formation of magmatic sulfide deposits in arcs by reduction of oxidized basalt. in GH Brown, PJ Jugo, CM Lesher & JE Mungall (eds), Abstracts, 11th International Platinum Symposium, 21-24 June 2010, Sudbury, Ontario, Canada. Ontario Geological Survey, Sudbury Canada, pp. 1 - 4, International Platinum Symposium, Sudbury Canada, 1/01/10.

Formation of magmatic sulfide deposits in arcs by reduction of oxidized basalt. / Tomkins, Andrew George; Rebryna, Kyle; Weinberg, Roberto Ferrez et al.

Abstracts, 11th International Platinum Symposium, 21-24 June 2010, Sudbury, Ontario, Canada. ed. / G H Brown; P J Jugo; C M Lesher; J E Mungall. Sudbury Canada : Ontario Geological Survey, 2010. p. 1 - 4.

Research output: Chapter in Book/Report/Conference proceeding › Conference Paper › Research › peer-review

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N2 - A region of magma mingling and mixing, containing magmatic sulfide mineralization, within a magmatic arc cross section in Hokkaido, Japan, is examined to explore the consequences of chemical equilibration between mantle-derived arc basalts and crust-derived graphite-bearing tonalites. Reduction of oxidized arc basalt, driven by buffering with contaminant graphite, is shown to be a viable mechanism for causing sulfide oversaturation.

AB - A region of magma mingling and mixing, containing magmatic sulfide mineralization, within a magmatic arc cross section in Hokkaido, Japan, is examined to explore the consequences of chemical equilibration between mantle-derived arc basalts and crust-derived graphite-bearing tonalites. Reduction of oxidized arc basalt, driven by buffering with contaminant graphite, is shown to be a viable mechanism for causing sulfide oversaturation.

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BT - Abstracts, 11th International Platinum Symposium, 21-24 June 2010, Sudbury, Ontario, Canada

A2 - Brown, G H

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PB - Ontario Geological Survey

CY - Sudbury Canada

T2 - International Platinum Symposium

Y2 - 1 January 2010

ER -

Formation of magmatic sulfide deposits in arcs by reduction of oxidized basalt

Abstract

Conference

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