Zobrazeno 1 - 10
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pro vyhledávání: '"G, La Spina"'
Publikováno v:
Nature Communications, Vol 9, Iss 1, Pp 1-14 (2018)
Volatiles such as water play a key role in magma ascent and ultimately triggering explosive eruptions. Here, the authors show that water-rich melts with water concentrations of 6–9 wt.% can ascend rapidly to the surface over the timescales of hours
Externí odkaz:
https://doaj.org/article/3c25b15cc6a44ee396c6aed2625ffcb5
Akademický článek
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Publikováno v:
Nature Communications, Vol 7, Iss 1, Pp 1-10 (2016)
The quantification of timing for crystallization and exsolution processes are fundamental to our understanding of basaltic magma ascent dynamics. Here, the authors constrain timings to show that plagioclase reaches equilibrium in 1-2 hours, whereas a
Externí odkaz:
https://doaj.org/article/94a22e7fd6e84b63be1e081fe3d731fc
Publikováno v:
Journal of Geophysical Research: Planets. 126
Publikováno v:
La Spina, G, Polacci, M, Burton, M & de'Michieli Vitturi, M 2017, ' Numerical investigation of permeability models for low viscosity magmas: application to the 2007 Stromboli effusive eruption. ', Earth and Planetary Science Letters . https://doi.org/10.1016/j.epsl.2017.06.013
Magma permeability is the most important factor controlling the transition between effusive and explosive styles during magma ascent at active volcanoes. When magma permeability is low, gas bubbles in the melt expand as the pressure decreases; above
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Publikováno v:
Nature Communications
Nature Communications, Nature Publishing Group, 2018, 9 (1), pp.art. 770. ⟨10.1038/s41467-018-02987-6⟩
Petrelli, M, El Omari, K, Spina, L, Le Guer, Y, La Spina, G & Perugini, D 2018, ' Timescales of water accumulation in magmas and implications for short warning times of explosive eruptions ', Nature Communications, vol. 9, no. 1, 770 . https://doi.org/10.1038/s41467-018-02987-6
Nature Communications, Vol 9, Iss 1, Pp 1-14 (2018)
Nature Communications, Nature Publishing Group, 2018, 9 (1), pp.art. 770. ⟨10.1038/s41467-018-02987-6⟩
Petrelli, M, El Omari, K, Spina, L, Le Guer, Y, La Spina, G & Perugini, D 2018, ' Timescales of water accumulation in magmas and implications for short warning times of explosive eruptions ', Nature Communications, vol. 9, no. 1, 770 . https://doi.org/10.1038/s41467-018-02987-6
Nature Communications, Vol 9, Iss 1, Pp 1-14 (2018)
Water plays a key role in magma genesis, differentiation, ascent and, finally, eruption. Despite the recognized crucial function of water, there are still several issues that continue to blur our view about its role in magmatic systems. What are the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b2d570476c2b2aace6d72e32883b0497
https://hal-univ-pau.archives-ouvertes.fr/hal-02146091
https://hal-univ-pau.archives-ouvertes.fr/hal-02146091
Autor:
Anastasia Foglia, M. Rantolo, Manuela Tomai, Rossella Palma, Cristina Panetta, Stefano Pontone, G. Gallo, M. Cremona, Marco Lauriola, G. La Spina
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::65095ff05cac8927ea4f8eb7c642b640
http://hdl.handle.net/11573/1123062
http://hdl.handle.net/11573/1123062
Publikováno v:
Earth and Planetary Science Letters. 426:89-100
The dynamics of magma ascent are controlled by the complex, interdependent processes of crystallisation, rheological evolution, gas exsolution, outgassing, non-ideal gas expansion and temperature evolution. Temperature changes within the conduit, in