Stress field change around the Mount Fuji volcano magma system caused by the Tohoku megathrust earthquake, Japan
- 12 January 2013
- journal article
- Published by Springer Science and Business Media LLC in Bulletin of Volcanology
- Vol. 75 (1)
- https://doi.org/10.1007/s00445-012-0679-9
Abstract
No abstract availableKeywords
This publication has 33 references indexed in Scilit:
- Simultaneous magma and gas eruptions at three volcanoes in southern Italy: An earthquake trigger?Geology, 2009
- Three-dimensional P- and S-wave velocity structures beneath the Japan Islands obtained by high-density seismic stations by seismic tomographyTectonophysics, 2008
- Volcanic activity influenced by tectonic earthquakes: Static and dynamic stress triggering at Mt. MerapiGeophysical Research Letters, 2007
- Volcanic eruptions following M ≥ 9 megathrust earthquakes: Implications for the Sumatra-Andaman volcanoesGeology, 2007
- SEISMIC TRIGGERING OF ERUPTIONS IN THE FAR FIELD: Volcanoes and GeysersAnnual Review of Earth and Planetary Sciences, 2006
- Deep low-frequency earthquake swarm in the mid crust beneath Mount Fuji (Japan) in 2000 and 2001Bulletin of Volcanology, 2005
- On the long‐term interaction among earthquakes: Some insight from a model simulationJournal of Geophysical Research, 2003
- Mechanical Coupling Between Volcanic Unrests and Large Earthquakes: A Review of Examples and Mechanisms.Journal of Geography (Chigaku Zasshi), 2002
- Role of carbon dioxide in the dynamics of magma ascent in explosive eruptionsBulletin of Volcanology, 1999
- Two‐way coupling between Vesuvius eruptions and southern Apennine earthquakes, Italy, by elastic stress transferJournal of Geophysical Research, 1998