Mechanism of the 1991 eruption of Hekla from continuous borehole strain monitoring
- 1 October 1993
- journal article
- Published by Springer Nature in Nature
- Vol. 365 (6448) , 737-740
- https://doi.org/10.1038/365737a0
Abstract
No abstract availableKeywords
This publication has 13 references indexed in Scilit:
- Emplacement of dikes, sills and crustal magma chambers at divergent plate boundariesPublished by Elsevier ,2003
- Anatomy of a basaltic volcanoNature, 1993
- Magma chamber deflation recorded by the global positioning system: The Hekla 1991 EruptionGeophysical Research Letters, 1992
- A Model for the 1989 Seismo-Volcanic Activity off Ito, Central Japan, Derived from Crustal Movement Data.Journal of Physics of the Earth, 1991
- Detection of a volcanic fracture opening in Japan using Global Positioning System measurementsNature, 1990
- Deformation from inflation of a dipping finite prolate spheroid in an elastic half‐space as a model for volcanic stressingJournal of Geophysical Research, 1988
- Ultrasonic measurements of Vp and Qp: relaxation spectrum of complex modulus on basalt meltsPhysics of the Earth and Planetary Interiors, 1985
- The Hekla eruption 1980–1981Bulletin of Volcanology, 1983
- Location of a magma reservoir beneath Hekla Volcano, IcelandNature, 1983
- The Hekla Eruption of 1970Bulletin of Volcanology, 1972