Slow waves trapped in a fluid-filled infinite crack: Implication for volcanic tremor

Author:

Ferrazzini Valerie,Aki Keiiti

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference33 articles.

1. Deep volcanic tremor and magma ascent mechanism under Kilauea, Hawaii;Aki;J. Geophys. Res.,1981

2. Aki, K., , P. G., Richards, , Quantitative Seismology: Theory and Methods, W. H. Freeman, San Francisco, 1980,

3. Source mechanism of volcanic tremor: Fluid-driven crack models and their application to the 1963 Kilauea eruption;Aki;J. Volcanol. Geotherm. Res.,1977

4. Observations of long-period earthquakes accompanying hydraulic fracturing;Bame;Geophys. Res. Lett.,1986

5. The interaction of Rayleigh and Stoneley waves in the ocean bottom;Biot;Bull. Seismol. Soc. Am.,1952

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