Causes and consequences of pressurisation in lava dome eruptions
- 1 August 1997
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 150 (3-4), 177-189
- https://doi.org/10.1016/s0012-821x(97)00109-x
Abstract
No abstract availableKeywords
This publication has 35 references indexed in Scilit:
- Pre-eruptive volatile content and degassing history of an evolving peralkaline volcanoJournal of Volcanology and Geothermal Research, 1996
- Water and the viscosity of andesite meltsChemical Geology, 1996
- Rheology of crystal‐bearing silicate melts: An experimental study at high viscositiesJournal of Geophysical Research: Solid Earth, 1995
- Magmatic Vapor Source for Sulfur Dioxide Released During Volcanic Eruptions: Evidence from Mount PinatuboScience, 1994
- Estimate of pyroclastic flow velocities resulting from explosive decompression of lava domesNature, 1993
- On the variations of flow rate in non-explosive lava eruptionsEarth and Planetary Science Letters, 1993
- Crumbling of dacite dome lava and generation of pyroclastic flows at Unzen volcanoNature, 1992
- Gas content, eruption rate and instabilities of eruption regime in silicic volcanoesEarth and Planetary Science Letters, 1991
- Crystallization history of Obsidian Dome, Inyo Domes, CaliforniaBulletin of Volcanology, 1989
- Effect of degassing on rheology of basaltic lavaNature, 1978