The role of gas percolation in quiescent degassing of persistently active basaltic volcanoes
- 15 December 2007
- journal article
- research article
- Published by Elsevier BV in Earth and Planetary Science Letters
- Vol. 264 (1-2), 46-60
- https://doi.org/10.1016/j.epsl.2007.08.028
Abstract
No abstract availableKeywords
This publication has 55 references indexed in Scilit:
- Non-Newtonian rheology of crystal-bearing magmas and implications for magma ascent dynamicsEarth and Planetary Science Letters, 2007
- Magmatic Gas Composition Reveals the Source Depth of Slug-Driven Strombolian Explosive ActivityScience, 2007
- Textural effects of steady state behaviour of the Stromboli feeding systemJournal of Volcanology and Geothermal Research, 2007
- Permeability‐porosity relationship: A reexamination of the Kozeny‐Carman equation based on a fractal pore‐space geometry assumptionGeophysical Research Letters, 2006
- Spectroscopic evidence for a lava fountain driven by previously accumulated magmatic gasNature, 2005
- Stromboli volcano (Aeolian Archipelago, Italy): An open window on the deep‐feeding system of a steady state basaltic volcanoJournal of Geophysical Research, 2003
- Factors controlling permeability-porosity relationships in magmaBulletin of Volcanology, 2001
- Endogenous magma degassing and storage at Mount EtnaGeophysical Research Letters, 1997
- Sulphur output and magma degassing budget of Stromboli volcanoNature, 1994
- Photoballistics of volcanic jet activity at Stromboli, ItalyJournal of Geophysical Research, 1974