Found inside – Page 14EARTHQUAKE , GENERAL * TECTONICS + EARTHQUAKE PREDICTION + EARTHQUAKE ... STUDIES OF THE MATSUSHIRO EARTHQUAKE SWARM EARTHQUAKE RESEARCH INSTITUTE 46 PAGES ... Found inside – Page 249Summary of the seismographic observation of Matsushiro swarm earthquakes. Bull. Earthquake Res. Inst., 46: 485—515. J.M.A., 1968. Report on the Matsushiro ... Found inside – Page 44The epicentral region of this swarm is in the immediate vicinity of the active zone in the 1965–1967 Matsushiro earthquake swarm . In both of these earthquakes some houses and go - downs suffered slight damages . Total number of felt ... Found inside – Page 175 - 1 Catalogue of literatures and documents on the Matsushiro earthquake swarm ( in Japanese ) , Review of Research for Disaster Prevention 143 , Science and Technology Agency , Japan National Research Center for Disaster Prevention ... Found inside – Page 137area Hagiwara , T. and T. Iwata , 1968 : Summary of the seismological observation of Matsushiro swarm earthquakes . Bull . Earthq . ... Ichikawa , M. , 1967 : Statistical study of the focal mechanism of Matsushiro earthquake swarm . Zisin ( J. The book focuses on the structure, composition, and characteristics of the earth's crust. Found inside – Page 202The phenomenon wherein an aftershock area or a focal region of earthquake swarm expands with time was also found in the cases of the Matsushiro earthquake swarm from 1965 to 1967 ( HAGIWARA and Iwata , 1968 ) , Izu - Oshima - kinkai ... Found inside – Page 59( 4 ) Slight subsidence occurred near B.M. 9341–9344 when the crustal upheaval occurred near B.M.9334-9337 . 3 . The Matsushiro Earthquake Swarm Another typical earthquake swarm is the Matsushiro earthquake swarm that began on ... Found inside – Page 73Center for Disas . Prev . ) ( 1967 ) Seismological data of Matusshiro earthquake swarm . Rev. Res . Disas . Prev . No.1 . NOGUCHI , K. ( 1967 ) Matsushiro earthquakes and hot springs . Chemistry and Chemical Industry ( Kagaku to Kogyo ) 20 ... Found inside – Page 106[2] A. NUR, Matsushiro, Japan, earthquake swarm: Confirmation of the dilatancy—fluid diffusion model, Geology 2 (1974), 217. Found inside – Page 207The above stated conditions for the intensive hydration reaction suggest that the earthquake swarms by the hydration ... of the numerical estimation : Matsushiro earthquakes Matsushiro earthquakeswarm is the quite remarkable example . Found inside – Page 1070Kisslinger , C. , 1968 , Energy density and the development of the source region of the Matsushiro earthquake swarm : Bull . Earthq . Res . Inst . v . Found inside – Page 399The variation with tp of the slope Ats / Atp for two selected events from the Matsushiro earthquake swarm . with the previous section , it appears that a porosity change Ac / c = . 15 is very reasonable when c = . 01 . Thus on the basis of the data ... In Matsushiro, central Japan, a series of more than 700,000 earthquakes occurred over a 2-year period (1965-1967) associated with a strike-slip faulting sequence. Found inside – Page 1344KASUGA , I . ( 1967 ) , Aspect on the Relation of Thermal Water and Matsushiro Earthquakes in Kagai Hot Spring Area ... KISSLINGER , C . ( 1975 ) , Process during the Matsushiro , Japan , Earthquake Swarm as Revealed by Leveling ... Found inside – Page 50745 The Japanese prediction program was first tested ( largely because of social pressures ) during the Matsushiro earthquake swarm . Found inside – Page 199204 Pure app!. geophys. , P. Reasenberg demonstrated that in Cascadia earthquakes are four times more likely to be foreshocks than in California. Found inside – Page xviMaster Events ' Earthquakes of Ms larger than 5.0 among the Matsushiro Earthquake Swarm of 1966 and 1967 (Table 1) were employed as master events. The accuracy of epicentre determination is 1 1 km. Fig. 1 shows differences between ... Found inside – Page 437Matsushiro Swarms The Matsushiro earthquake swarms (Central Honshu, Japan) began on 3 August 1965 with the earthquakes clustering within a 5-km radius zone ... Found inside – Page 263Investigations in Kamchatka for purposes of earthquake prediction have included detailed ... and deep drilling in the Matsushiro earthquake swarm area . Found inside – Page 544J. Geophys. Res., 68: 2791–2815. Suyehiro, S., 1962. Deep earthquakes in the Fiji region. Pap. Meteorol. Geophys., 13: 216–238. Suyehiro, S., 1968. Change in earthquake spectrum before and after the Matsushiro swarm. Pap. Meteorol. Found inside – Page 399The variation with tp of the slope Ats / Atp for two selected events from the Matsushiro earthquake swarm . with the previous section , it appears that a porosity change Ac / c = . 15 is very reasonable when c = . 01 . Thus on the basis of the data ... Found inside – Page 50AMBRASEYs, N. N.; TCHALENko, J.S. The Dasht-e Bāyāz earthquake of 31 August 1968: general field report. May 1969. ... HAGIwARA, T.; Iwata, T. Summary of the seismographic observation of Matsushiro earthquake swarms. Bull. Earthq. Found inside – Page 915is the same for Asadha Volcano and Matsushiro Wolcano (Japan): respectively 50–60 and approximately 50 kif [21]. A Similar value (80 kno) is given for the area of the epicentral zone of a brief earthquake swarm near the extinct Aag Volcano ... Found inside – Page 310With respect to earthquake swarms, MOGI (1967b) investigated decays in event ... rate were observed in the Matsushiro earthquake swarm, Japan, in 1965-1967. Found inside – Page 486Kasahara , K. , 1970 , The source region of Matsushiro swarm earthquakes ... Processes during the Matsushiro , Japan , earthquake swarm as revealed by ... Found inside – Page 10Amplification of Earthquake Ground Motion in Surface Ground Layers Deriving from the Observation of the Matsushiro ... by analyzing the earthquake records of the Matsushiro Earthquake Swarm observed at many points under the surface ... Found inside – Page 22... punctuated but more or less continuous earthquake - swarm activity since 1978 ... as in the cases of Matsushiro , Japan , and Long Valley , California . This paper presents recent advancement in and applications of TOUGH-FLAC, a simulator for multiphase fluid flow and geomechanics. Found inside – Page 391The Matsushiro earthquake swarm began in August 1965 and continued for more than three years . The activity first occurred in a very small area and then ... Found inside – Page 130Part of this study was conducted under the project of Earthquake Research Institute , University of Tokyo : Prediction Study on ... Mogi , K. , 1988 , The mechanism of the occurrence of the Matsushiro earthquake swarm in central Japan and in ... Found inside – Page 363The total intensity change observed during the Matsushiro earthquake swarm ( 1965-1970 ) was the first reliable example of tectonomagnetic effects as revealed by proton precession magnetometers ( Yamazaki and Rikitake , 1970 ) . First tested ( largely because of social pressures ) during the Matsushiro swarm focuses on the structure, composition and!, 1967: Statistical study of the focal mechanism of Matsushiro earthquake swarms - downs slight... ) during the Matsushiro... Found inside – Page 544J Summary of the focal of! 1967: Statistical study of the focal mechanism of Matsushiro earthquake swarms 1967 ) Seismological data of Matusshiro earthquake.! Advancement in and applications of TOUGH-FLAC, a simulator for multiphase fluid flow and geomechanics general field.! In Cascadia earthquakes are four times more likely to be foreshocks than California! 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