Carbonate-derived CO2 purging magma at depth: Influence on the eruptive activity of Somma-Vesuvius, Italy-Reference-Cited by-同舟云学术

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Carbonate-derived CO2 purging magma at depth: Influence on the eruptive activity of Somma-Vesuvius, Italy

Published:2011-10 Issue:1-2 Volume:310 Page:84-95
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Dallai Luigi,Cioni Raffaello,Boschi Chiara,D'Oriano Claudia

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference82 articles.

1. Experimental determination of oxygen isotope fractionations between CO2 vapor and sodamelilite melt;Appora;Geochim. Cosmochim. Acta,2003

2. Seismic evidence of an extended magmatic sill under Mt. Vesuvius;Auger;Science,2001

3. Geochemical and isotopic (Nd–Pb–Sr–O) variations bearing on the genesis of volcanic rocks from Vesuvius, Italy;Ayuso;J. Volcanol. Geotherm. Res.,1998

4. Assimilation and metamorphism at basalt-limestone contact, Tokatoka, New Zealand;Baker;Mineral. Mag.,1980

5. Metamorphic carbonate ejecta from Vesuvius plinian eruptions: evidence of the occurrence of shallow magma chambers;Barberi;Bull. Volcanol.,1980

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2. Experimental re-melting of a continental crust: probing the deep storage zone of Campi Flegrei and Vesuvius magmas;Contributions to Mineralogy and Petrology;2024-04-09

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