Co-Seismic Displacements of the 1995 Hyogo-Ken Nanbu Earthquake Manabu Hashimoto,* Takeshi Sagiya, Hiromichi Tsuji, Yuki Hatanak
J. Phys. Earth, 44, 255-279, 1996 Co-seismic Displacements of the 1995 Hyogo-ken Nanbu Earthquake Manabu Hashimoto,* Takeshi Sagiya, Hiromichi Tsuji, Yuki Hatanaka, and Takashi Tada GeographicalSurvey Institute, Tsukuba 305, Japan We presentco-seismic displacements of the Hyogo-kenNanbu earthquake of January 17, 1995,detected by continuousGPS (Global Positioning System) observation, campaign type GPS survey and leveling. Continuous GPS observationgives a consistentpattern of displacementswith thoseexpected from a right lateralslip on a NE-SWtrending vertical fault in far field:stations about 50km east and west of the epicentermoved toward the epicenterby about4 cm,while stations north and south movedaway from the epicenter.By comparing with line lengthsobtained by geodoliteabout 10 yearsago, the campaigntype GPS revealed most controlpoints on AwajiIsland moved to the southwestor south,which may be attributedto the movementof the NojimaFault whichcut the surface.On the other hand, controlpoints northwest of the Rokkofault systemmoved toward the northeastand thoseon theother side moved slightly to the west,in and aroundKobe. Leveling data revealed upliftof 19cm on the northwesternside of theSuma Fault, a memberof the Rokko faultsystem, and subsidence of 7 cmjust east of this fault. Furthermore,uplift of about 5 cmwas observedin the centralpart of Kobe City, and subsidenceof 5 cm was detectedeast of Kobe. There is no significantgap in horizontaland vertical displacementsaround the northernextension of the NojimaFault, which implies a complicatedrupture process of this event.Leveling on the east coastof AwajiIsland revealed a significantuplift of about 20 cm with slight subsidenceat both edgesof this upliftregion during the past 20 years. By fittingthe abovegeodetic data, we searchedfor an optimalset of parametersof a dislocationmodel.
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