A quantitative approach to the dike intrusion process inferred from a joint analysis of geodetic and seismological data for the 1998 earthquake swarm off the east coast of Izu Peninsula, central Japan

Author:

Morita Yuichi1,Nakao Shigeru1,Hayashi Yoshinari1

Affiliation:

1. Earthquake Research Institute; University of Tokyo; Tokyo Japan

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

Reference51 articles.

1. Imaging magma transport during the 1997 seismic swarm off the Izu Peninsula, Japan;Aoki;Science,1999

2. Geology of the Higashi-Izu monogenetic volcano group;Aramaki;Bull. Earthquake Res. Inst. Univ. Tokyo,1977

3. Resolving the discrepancy between geodetic and seismic fault models for the 1989 Loma Prieta, California Earthquake;Arnadottir;Bull. Seismol. Soc. Am.,1992

4. The effect of solidification on fluid-driven fracture, with application to bladed dykes;Bolchover;Proc. R. Soc. London, Ser. A,1999

5. Seismic activity associated with the September 1977 deflation of the Krafla Central volcano in northeastern Iceland;Brandsdottir;J. Volcanol. Geotherm. Res.,1979

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