Magma flow between summit and Pu‘u ‘Ō‘ō at K̄lauea Volcano, Hawai‘i
Author:
Affiliation:
1. Department of Earth Science; Keith-Wiess Geological Lab, Rice University; Houston Texas USA
2. Now at Istituto Nazionale di Geofisica e Vulcanologia; Sezione di Pisa Pisa Italy
Funder
NSF
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Reference65 articles.
1. Identifying elements of the plumbing system beneath K̄lauea Volcano, Hawaii, from the source locations of very-long-period signals;Almendros;Geophys. J. Int.,2002
2. Magma flow through elastic-walled dikes;Bokhove;Theor. Comput. Fluid Dyn.,2005
3. Tectonic stress and magma chamber size as controls on dike propagation: Constraints from the 1975-1984 Krafla rifting episode;Buck;J. Geophys. Res.,2006
4. High magma storage rates before the 1983 eruption of K̄lauea, Hawaii;Cayol;Science,2000
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