CO2-crystal wettability in potassic magmas: implications for eruptive dynamics in light of experimental evidence for heterogeneous nucleation-Reference-Cited by-同舟云学术

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CO2-crystal wettability in potassic magmas: implications for eruptive dynamics in light of experimental evidence for heterogeneous nucleation

Published:2017-02-01 Issue:2 Volume:209 Page:688-694
ISSN:0956-540X
Container-title:Geophysical Journal International
language:en
Short-container-title:

Author:

Sottili Gianluca,Fanara Sara,Silleni Aurora,Palladino Danilo M.,Schmidt Burkhard C.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/gji/article-pdf/209/2/688/10868079/ggx039.pdf

Reference41 articles.

1. Unusually large magmatic CO2 gas emissions prior to a basaltic paroxysm;Geophys. Res. Lett.,2010

2. The control of magma volatile content and chamber depth on the mass erupted during explosive volcanic eruptions;J. geophys. Res.,1997

3. Fluids in the lithosphere, 1. Experimentally-determined wetting characteristics of CO2-H2O fluids and their implications for fluid transport, host-rock physical properties, and fluid inclusion formation;Earth planet. Sci. Lett.,1987

4. Magma–carbonate interaction processes and associated CO2 release at Merapi volcano, Indonesia: insights from experimental petrology;J. Petrol.,2010

5. Contact angle and stability of interfacial nanobubbles;Langmuir,2009

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1. Decarbonation and clast dissolution timescales for short-term magma‑carbonate interactions in the volcanic feeding system and their influence on eruptive dynamics: Insights from experiments at atmospheric pressure;Chemical Geology;2023-11

2. Magma–rock interactions: a review of their influence on magma rising processes with emphasis on short-timescale assimilation of carbonate rocks;Geological Society, London, Special Publications;2022-05-31

3. Dynamics of degassing in evolved alkaline magmas: Petrological, experimental and theoretical insights;Earth-Science Reviews;2020-12

4. Magmatic stoping during the caldera-forming Pomici di Base eruption (Somma-Vesuvius, Italy) as a fuel of eruption explosivity;Lithos;2020-10

5. CO 2 favours the accumulation of excess fluids in felsic magmas;Terra Nova;2020-09-28

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