7-3 2004年新潟県中越地震
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1 04 Mid Niigata earthquake Earthquake Research Institute, University of Tokyo M M M M M.9 30km M ) 2 RMS P S P 3 S km 17km 3 M6 km 27 M6.1 Double-Difference 2)
2 4 km 3 4 km (M6.8) (18:34 M6.) /27 6 / ,000m tear fault km 2mm/ 1mm/ A-A' ) M
3 27 40 M ) Takeda, T., H. Sato, T. Iwasaki, N. Matsuta, S. Sakai, T. Iidaka and A. Kato, Crustal structure in the northern Fossa Magna region, central Japan, from refraction/wide-angle reflection data, Earth Planets Space (04). 2) Zhang, H., and C., Thurber, Double-Difference Tomography: the method and its application to the Hayward Fault, California, Bulletin of the Seismological Society of America, 93, (03). 3) 2 (1992). 4) : (04) ) : 1 132p ) : 1 4p ) : 1 177p ) 799p ) :, 60p, (02). ) :1:2,000 D.1-No ) : : (Wed, 17 Nov 04 08:14: ), 12) p.1992.
4 138 00' 38 00' ' ' ' 37 30' 37 00' 36 30' ' ' ' ' 1 Fig.1Location of permanent stations ( ) and temporal stations(, ) Fig.2Model of velocity structure (W:thick line, E:thin line).
5 Fig.3Hypocentral distribution. The main shock ( ) and some large aftershocks ( ) are shown.
6 4 Double-Difference Zhang ;Thurber, 03 P km/s Fig.4Depth section showing the P wave velocity structure and the relocated aftershocks derived from the double-difference tomography (Zhang and Thurber, 03). Gray circles denote the locations of the aftershocks, and the color contour shows the P wave velocity.
7 Mw 30 km km 1 m 9.0 **18 Nm 6.6 km km 0. m 3.0 **18 Nm 6.3 Fig.Change of Coulomb stress due to the main shock and the largest aftershock.
8 6 a: b: :04 : Fig.6Bouguer anomaly map of Niigata and southern Tohoku district and the hypocentral location of the 04 Mid Niigata earthquake. a: Shibata-Koide tectonic line, b: Kashiwazaki-Choshi tectonic line, red star: hypocenter of the 04 Mid Niigata earthquake, Blue star: hypocenter of the 03 Northern Miyagi earthquake, Bouguer anomalies are after Geological Survey of Japan (1992). 7 1: M6.82: M6.33: M6.04: M6.: M6.1a: b: c: 6)7)8) 9 4 Fig.7Geological structure and hypocentral distribution around the source area of the 04 Mid Niigata earthquake. 1: Main shock (October 23, 17:6' M6.8), 2: Aftershock (Oct. 23, 18:03' M6.3), 3: Aftershock (Oct. 23, 18:11' M6.0), 4: Largest aftershock (Oct. 23, 18:34 M6.), : Aftershock (Oct. 27, :40 M6.1), a: Obirou fault, b: Mikamachi fault, c: Suwa-toge flexure. Geological map is compiled after ), 6), 7) and 8), active fault is 9) and ), tilting of river terraces is after 4).
9 , 12 Fig.8Schematic diagram showing the crustal structure across the source faults of the 04 Mid Niigata earthquake. Thick solid line represents an estimated source fault. Circle: aftershock, triangle: site of drill hole projected onto cross section. The data of drill holes is after ) and 12). 9 Fig.9Schematic diagram showing the 3D view of the source faults (not in exact scale).
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