A 667 year record of coseismic and interseismic Coulomb stress changes in central Italy reveals the role of fault interaction in controlling irregular earthquake recurrence intervals
Current studies of fault interaction lack sufficiently long earthquake records and measurements of fault slip rates over multiple seismic cycles to fully investigate the effects of interseismic loading and coseismic stress changes on the surrounding fault network. We model elastic interactions betwe...
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Veröffentlicht in: | Journal of geophysical research. Solid earth 2017-07, Vol.122 (7), p.5691-5711 |
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Sprache: | eng |
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