Authors:
SINGH SK
ORDAZ M
MIKUMO T
PACHECO J
VALDES C
MANDAL P
Citation: Sk. Singh et al., IMPLICATIONS OF A COMPOSITE SOURCE MODEL AND SEISMIC-WAVE ATTENUATIONFOR THE OBSERVED SIMPLICITY OF SMALL EARTHQUAKES AND REPORTED DURATION OF EARTHQUAKE INITIATION PHASE, Bulletin of the Seismological Society of America, 88(5), 1998, pp. 1171-1181
Citation: T. Mikumo et al., DYNAMIC RUPTURE OF ASPERITIES AND STRESS CHANGE DURING A SEQUENCE OF LARGE INTERPLATE EARTHQUAKES IN THE MEXICAN SUBDUCTION ZONE, Bulletin of the Seismological Society of America, 88(3), 1998, pp. 686-702
Citation: Gc. Beroza et T. Mikumo, SHORT SLIP DURATION IN DYNAMIC RUPTURE IN THE PRESENCE OF HETEROGENEOUS FAULT PROPERTIES, J GEO R-SOL, 101(B10), 1996, pp. 22449-22460
Citation: T. Mikumo et T. Miyatake, HETEROGENEOUS DISTRIBUTION OF DYNAMIC STRESS DROP AND RELATIVE FAULT STRENGTH RECOVERED FROM THE RESULTS OF WAVE-FORM INVERSION - THE 1984 MORGAN-HILL, CALIFORNIA, EARTHQUAKE, Bulletin of the Seismological Society of America, 85(1), 1995, pp. 178-193
Authors:
MIKUMO T
HIRAHARA K
TAKEUCHI F
WADA H
TSUKUDA T
FUJII I
NISHIGAMI K
Citation: T. Mikumo et al., 3-DIMENSIONAL VELOCITY STRUCTURE OF THE UPPER CRUST IN THE HIDA REGION, CENTRAL HONSHU, JAPAN, AND ITS RELATION TO LOCAL SEISMICITY, QUATERNARY ACTIVE VOLCANOS AND FAULTS, Journal of Physics of the Earth, 43(1), 1995, pp. 59-78
Citation: E. Fukuyama et T. Mikumo, DYNAMIC RUPTURE ANALYSIS - INVERSION FOR THE SOURCE PROCESS OF THE 1990 IZU-OSHIMA, JAPAN, EARTHQUAKE (M = 6.5), J GEO R-SOL, 98(B4), 1993, pp. 6529-6542