Volatiles in High-K Magmas from the Western Trans-Mexican Volcanic Belt: Evidence for Fluid Fluxing and Extreme Enrichment of the Mantle Wedge by Subduction Processes-Reference-Cited by-同舟云学术

Volatiles in High-K Magmas from the Western Trans-Mexican Volcanic Belt: Evidence for Fluid Fluxing and Extreme Enrichment of the Mantle Wedge by Subduction Processes

Published:2008-08-12 Issue:9 Volume:49 Page:1589-1618
ISSN:1460-2415
Container-title:Journal of Petrology
language:en
Short-container-title:

Author:

Vigouroux Nathalie,Wallace Paul J.,Kent Adam J. R.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/petrology/article-pdf/49/9/1589/16669110/egn039.pdf

Reference129 articles.

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3. CO2 contents and formation pressures of some Kilauean melt inclusions;Anderson;American Mineralogist,1993

4. Melt inclusions from Volcan Popocatepetl and Volcan de Colima, Mexico: Melt evolution due to vapor-saturated crystallization during ascent;Atlas;Journal of Volcanology and Geothermal Research,2006

5. Volatile diffusion in silicate melts and its effects on melt inclusions;Baker;Annals of Geophysics,2005

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