Skarn xenolith record crustal CO2 liberation during Pompeii and Pollena eruptions, Vesuvius volcanic system, central Italy

Limestone assimilation and skarn formation are important processes in magmatic systems emplaced within carbonate-rich crust and can affect the composition of the magma and that of associated volcanic gas. In this study we focus on marble and calc-silicate (skarn) xenoliths from contact reactions bet...

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Bibliographic Details
Published in:	Chemical geology Vol. 415; pp. 17 - 36
Main Authors:	Jolis, E.M., Troll, V.R., Harris, C., Freda, C., Gaeta, M., Orsi, G., Siebe, C.
Format:	Journal Article
Language:	English
Published:	Elsevier B.V 15-11-2015
Subjects:	Assimilation C and O isotopes Carbon dioxide Carbonates CO2 emission Contact Earth Science with specialization in Mineral Chemistry, Petrology and Tectonics Geovetenskap med inriktning mot mineralogi, petrologi och tektonik Magma Magma-carbonate interaction Marble Marble and skarn xenoliths Surface layer Texture Vesuvius volcanic system Vesuvius volcanic system C and O isotopes Magma–carbonate interaction CO2 emission Marble and skarn xenoliths
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