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1 * Damage distributions and hypocenters of Tenmei-Sagami earthquake and Kaei-Odawara earthquake Tomiichi UETAKE R&D Center, Tokyo Electric Power Company, 4-1, Egasaki-cho, Tsurumi-ku, Yokohama, Japan Atsuko NOGUCHI Global Environmental Policy Group Environment Department, Tokyo Electric Power Company 1-1-3, Uchisaiwai-cho, Chiyoda-ku, Tokyo, Japan Misao NAKAMURA Information Service for Disaster Prevention, 230-7, Miroku-cho, Sakura Chiba, Japan The seismic intensity distribution of the 1782 Tenmei-Sagami earthquake and the 1853 Kaei-Odawara earthquake were re-examined using historical documents in order to re-evaluate the location and magnitude of these events. The 1782 Tenmei-Sagami earthquake was estimated to have occurred in Kanagawa-Yamanashi border area with magnitude of 6.8 to 7.0. The 1853 Kaei-Odawara earthquake was estimated to have occurred in the north edge of the Ashigara plane with magnitude of 6.6 to 6.8. Keywords: Tenmei-Sagami earthquake, Kaei-Odawara earthquake, Earthquake damage distribution, Seismic Intensity Inversion, Hypocenter. 1 M (M7.0)1782 (M7.0)1853 (M6.7) 3 (1993) (2003)3 (2008) (1984) * : misao@ba2.so-net.ne.jp 5 45km M 7 (2003) (1986) (1997) (1993) M 7 5 M (1977) (2003) () M6.7 (1993) (1993)
2 (1993) 5 M 7 (1984) (2005) 1995 K-NETKik-net (2003) (2003) (2002) (1999) (2001) (2006)(2009) (1782 M7) (1853 M6.7) (2003)() () 1 2 ( 2) ( ) (2004) E e 2.3 ( ()) M7 3( ) ( ) 2.4 茨 ( )
3 ( 廻 ) ( ) 45 () () () 溢 () 溢 ()()( ) () () () () ( ) () () ( ) () () ( ) () ( ) () 6 爺 () () () 800 ( 1992) () 6 () ( )
4 () ()() 6 () 5 ( pp) 2.4 ()() 19 () 61 32% 6 ( ) () 迄 () () > ( 24 ) 15.2% 6 35km () 100km 5 (1984) 1 40 () 2.4 (20:30 ) (01:20 ) 2.3 () 124 ( )( )()( )( ) ( )()
5 ( ) % 茨 溢 () () () 4.5 ( ) 迄 () () () 45 () 迄 () () >5 15 ( 翰 )() ( ) () % 56 (Appendix ) %71% 7 ( ) % 6 67 ( ) () () 5 6 ( ) 6 ()
6 - 44 -
7 2 6 迄 () ()() ()() >5 ( )
8 3-46 -
9 4 6 3 (2003) M 4 14 (x) (M) (I) (1)
10 (1) ((2003) () >(5 )(e, E ) M (2)(1969) 5 S5 M (2) () km M km M 7.0 (1) 65km20km ( 8 ) 6 42 km30 km 20km M M6.8 8 (3) I I M M6.8M7.0 RMS I I N (3) ( 4 )()() () %
11 5 30km M km M ( 8 ) 36 km24 km 20km 10 M M (1) M km M6.6 M (2005) () 5 (2003) 11 (2003) M6.8M7.0 M6.6M6.8 (1782/8/23)(01:20 )(20:30 ) (1853/3/11)(09:40 ) 6 7 茨
12 M km, 1 4 M M
13 9-4 M km, 3 M M
14 10-4 M () (2003) () ( )
15 Qs ( ) 芦 1984 ( ) ( 16 ) ( nankai/16/sankousiryou2_2.pdf) 2002 () Appendix ( ) 撰 () () ( ) () () 1 : 2 ( ()1941) 2 : (() 1979) 3 : 3 ( ()1983) 4 : ( ()1989) 5 : ( ()1993) 6 : (() 1998) 7 : ( ()1999) 8 : ( ()2002) 9 : ( ()2005) 10 : ( ()2008) 1 : (()1951) 2 : 5 1( ()1987) 3 : ( ()1989) 4 : ( ()1993) 5 : (() 1998) 6 : ( ()1999) 7 : ( ()2002) 8 : ( ()2005) 9 : ( ()2008)
16 1.1 p.53 茨 廻 E 2-52 e E () E E 溢 ()() 兎 這 S () 廟 廟 E E
17 E ( ) > E 2-51 > E 迄 () > > E 迄 辻 e
18 e e E > () E E E > S E 迄 e E %
19 () 迄 () > () > () 迄 () > > > > > > > > > > 樋 迄 > E E E 2-51 S E e S e () E
20 2.1 p.53 茨 茨 e 喰 e E E E E E E e e 溢 榊 榊 E E 汲 E E E E E E 迄 E E S E 迄 E 迄 E 迄 > 迄 釜
21 > 翰 廻 > % % > % % % % > > > % > > >5 2-9 厩
22 >5 2-3 > 迄 翰 > 薩 牌 牌 厩 牌 牌 >
23 3 > > 廻 > > > > E E E e S 迄 E e 1-20 E e 1-20 e
24 E 竈 竈 E > > 迄 璙 e E e E e
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20 * Re-Evaluation of Isoseismal Maps and Magnitudes from Two Big Earthquakes along the Subduction Zone of Kyushu and Ryukyu Islands Early in the 20th Century Masayuki TAKEMURA, Katsuhisa KANDA Kobori
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JR東日本会社要覧2012-2013
Technology Planning Department Frontier Service Development Laboratory Advanced Railway System Development Center Safety Research Laboratory Disaster Prevention Research Laboratory Technical Center Environmental
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5 6 7 Seismic observation station Agency Seismic intensity South- North (NS) Maximum acceleration (Gal ) East-West (EW) Vertical (UD) Combining threecomponent Epicentral distance (km) Kawaguchi* JMA 7
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経済論集 ４６‐２（よこ）（Ｐ）☆／２．三崎
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30 2015 51-62 2015/01/17 2015/03/31 1914 * Literature Survey on Damage of Akita Mining College due to the 1914 Akita-Senboku Earthquake Toshihiko MIZUTA Center for Regional Development, Akita University
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30 2015 1-22 2014/11/25 2015/03/11 * Report on the Field Survey for the Memorial Matters from the 1923 Great Kanto Earthquake at Minami-Ashigara City in Kanagawa Prefecture, Japan Masayuki TAKEMURA Disaster
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1793 Detailed Distributions of Seismic Intensity and Tsunami Heights of the Kansei off Miyagi Prefecture Earthquake of February 17, 1793 Yuichi NAMEGA
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* Coseismic and postseismic coastal environment changes caused by the 1703 Genroku Kanto Earthquake in the southern part of Boso Peninsula, central Japan Jun Muragishi Graduate School of Urban Environmental
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http://www.zendanren.or.jp 樽 todanko@todanko.or.jp http://www.todanko.or.jp dandan@nakadan.or.jp http://www.nakadan.or.jp/home/ seidanko@galaxy.ocn.ne.jp http://www17.ocn.ne.jp/~seidanko/index.html nandanko@jasmine.ocn.ne.jp
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Annuals of Disas. Prev. Res. Inst., Kyoto Univ., No. 48 A, 2005 1. 2004 26 9 4,000m 28 8.7 2. 2004 12 26 M9.0 6cm ( 1,600km) ( 6,000km) 1900 Table 23 2 150 60 2 22 7 72 7,530 11 (1) 1755 62,000 (2) 1782
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Time Variation of Earthquake Volume and Energy-Density with Special Reference to Tohnankai and Mikawa Earthquake Akira IKAMi and Kumizi IIDA Departmen
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MSS mitomi@edm.bosai.go.jp matsuoka@edm.bosai.go.jp yamazaki@edm.bosai.go.jp taniguchi@manage.nitech.ac.jp 1 MSS MSS 2 2 1 m MSS CCT CCT Fig.1 CCT b02-b0 b0-b0b-b b-b1 CCT Landsat/TM MSS S/N 21x21 21x21
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