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Shizuoka-Seibu earthquake, 1981
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1-6 OF 6 RESULTS FOR
Shizuoka-Seibu earthquake, 1981
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Journal Article
Seismicity and waveforms of the microearthquakes before and after the Shizuoka-Seibu earthquake, central Japan Available to Purchase
Publisher: Seismological Society of America
Published: 01 April 1984
Bulletin of the Seismological Society of America (1984) 74 (2): 605–620.
...Mizuho Ishida; Masakazu Ohtake Abstract Investigating the foreshock-main shock-aftershock sequence of the Shizuoka-Seibu earthquake ( M = 2.8, 16 January 1981), central Japan, we found evidence that suggests high stress conditions for the foreshock period. The source dimension of the main shock...
Journal Article
Index to volume 74 Available to Purchase
Publisher: Seismological Society of America
Published: 01 December 1984
Bulletin of the Seismological Society of America (1984) 74 (6): 2727–2745.
... . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Earthquake, Central Japan, Seismicity and Waveforms of the Microearthquakes Before and After the Shizuoka-Seibu, by Mizuho Ishida and Masakazu Ohtake . . . . . . . . . . . . . . . . . . . . Earthquake, Foreshock and Aftershock Activity of the 1976 Mesa de Andrade, Mexico, by J. Javier Gonzales, F. Alejandro...
Journal Article
Characteristic Earthquake Model and Seismicity around Late Quaternary Active Faults in Japan Available to Purchase
Publisher: Seismological Society of America
Published: 01 June 2012
Bulletin of the Seismological Society of America (2012) 102 (3): 1041–1058.
... of large interplate earthquakes ( Singh et al. , 1983 ; Davison and Scholz, 1985 ; Papadopoulos et al. , 1993 ; Ishibe and Shimazaki, 2009 ). The uniform‐slip model ( Sieh, 1981 ) and the maximum‐magnitude model ( Wesnousky et al. , 1983 ) are variations of the characteristic earthquake model...
Journal Article
Author index Available to Purchase
Publisher: Seismological Society of America
Published: 01 December 1993
Bulletin of the Seismological Society of America (1993) 83 (6B): 2241–2326.
... and after the JameDE JarpS Shizuoka-Seibu earthquake, Central Japan 74, 2, 605-620, April 84 JarpSP JennPC -80 2177 IsraelssonH, JepsDC JeyaM Correlation of waveforms from closely spaced regional events JihRS JimeE 80, 6, 2177-2193, December 90 -75 1225 Iwan WD, Moser MA, Peng CY, Some observations...
Journal Article
Key word index Available to Purchase
Publisher: Seismological Society of America
Published: 01 December 1993
Bulletin of the Seismological Society of America (1993) 83 (6B): 2059–2240.
... size fault inf GariJ -80 0870 2102 BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA of the 1983 Borah Peak EARTHQUAKE with some considerations for s MachMN -77 0771 he 1979 Imperial Valley of the 1983 Borah Peak EARTHQUAKE, California / Geodetic measure LangJ -73 1203 fter the Shizuoka-Seibu he 1986...
Book: The Geology of Japan
Series: Geological Society, London, Geology of Series
Publisher: The Geological Society of London
Published: 01 January 2016
DOI: 10.1144/GOJ.14
EISBN: 9781862397064
... earthquake of M = 7.1; 1961 Kita-mino earthquake of M = 7.0; 1978 Izu-Oshima-kinkai earthquake of M = 7.0; 1984 Nagano-ken-seibu earthquake of M = 6.8; 1995 Kobe (Hyogo-ken-Nanbu) earthquake of M = 7.3; 2000 Tottori-ken-seibu earthquake of M = 7.3; 2004 Niigata-ken-Chuetsu earthquake of M = 6.8...
Abstract Chapter 7 introduced the plate configuration in and around the Japanese islands, particularly with respect to the deep seismic structure and associated seismicity. This chapter overviews the shallow seismicity in Japan, with a particular focus on inland active faulting from the viewpoint of earthquake geology. This is followed by a consideration of the long-term earthquake forecasting and seismic hazard assessment research that has been accelerated since the 1995 Kobe earthquake emphasizing several of the more important current issues such as the presence of hidden faults, the effects of fault segmentation, sequential rupture and seismic cycles, as well as time dependency due to stress perturbation.