Magma ascent mechanisms in the transition regime from solitary porosity waves to diapirism
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Magma ascent mechanisms in the transition regime from solitary porosity waves to diapirism ; year:2020 ; pages:1-14
Solid earth discussions ; (2020), 1-14
- Creator
- DOI
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10.5194/se-2020-124
- URN
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urn:nbn:de:101:1-2020080618354326203414
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 11:00 AM CEST
Data provider
This object is provided by:
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Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
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Modelling chemical advection during magma ascent
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Rapid accumulation and ascent precedes caldera forming eruption of low viscosity magma
Magma ascent mechanisms in the transition regime from solitary porosity waves to diapirism
Modelling chemical advection during magma ascent
Modelling chemical advection during magma ascent
Numerical modeling of magma ascent through the lithosphere
Magnetosonic Solitary Waves
Multiscaled Solitary Waves
Ascent-driven differentiation: a mechanism to keep arc magmas metaluminous?
Ascent-driven differentiation: a mechanism to keep arc magmas metaluminous?
Rapid magma ascent beneath La Palma revealed by seismic tomography
Model for the origin, ascent, and eruption of lunar picritic magmas
Viscous flow of magmas from Unzen volcano, Japan : implication for magma mixing and ascent = Viskositäten von Magmen des Unzen Vulkans, Japan