2016年熊本地震 地震調査委員会の報告
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1 プレス ブリーフィング 熊本地震と日本の地震活動 The 2016 Kumamoto Earthquake and Japanese Seismic Activity 東京大学地震研究所地震予知研究センター平田直 2016/4/27 FPCJ プレスプレス ブリーフィング 1
2 益城町で震度 7 を記録した熊本地方の二つの地震 Two large earthquakes with seismic intensity 7 at Mashiki town in Kumamoto The April 14, 2016 earthquake with a magnitude (M) 6.5 The April 16, 2016 earthquake with an M 7.3 2
3 Evaluation of the 2016 Kumamoto earthquake The 288 th earthquake committee (Special) 2016 April 15 An earthquake with a magnitude of 6.5 (preliminary) occurred at a depth of 10 km at 21:26 on April 14 in Japan Standard Time (Japan Local Time = UT + 9 hr). Seismic intensity of 7 in Japan Meteorological Agency (JMA) scale was observed in Kumamoto Prefecture and damages are reported. As of the time when the report was issued, the seismic activity undergoes as mainshock-aftershock sequence. The maximum aftershock with a magnitude 6.4 (preliminary) occurred at 00:03 on 15 th with the maximum intensity of 6+ in JMA scale (as of 18:00 on April 15 th ). Aftershocks are active although decaying forming 20-km-long area with a NE-SW direction. 3
4 Evaluation of the 2016 April 16 th Kumamoto earthquake The 289 th committee (Special) An earthquake with a magnitude 7.3 (preliminary) occurred at a depth of 10 km at 01:25 on April 16 in JST. Seismic intensity of 6+ *in JMA scale was observed in Kumamoto Prefecture. An earthquake with a magnitude 6.5 (preliminary) occurred at a depth of 10 km at 21:26 on April 14 in JST. Seismic intensity of 7 was observed in Kumamoto Prefecture and damages are reported. Aftershock activity is prominent in a 30-km-long area and in neighboring areas of Aso district in Kumamoto prefecture and Oita prefecture. *) The intensity has been corrected to 7 4
5 Seismic Intensities: JMA scale vs MM scale The Japan Meteorological Agency seismic intensity scale is a seismic scale used in Japan and Taiwan to measure the intensity of earthquakes. It is measured in units of shindo ( 震度, seismic intensity, lit. "degree of shaking"). Modified Mercalli Intensity Scale is determined from effects on people, human structures, and the natural environment. is used in US, Korea 2016/4/27 FPCJ プレスプレス ブリーフィング 5
6 Seismic Intensity in JMA scale Seismic intensity describes the scale of the ground motion at a particular location. It varies with the distance from the epicenter and the surface geology at each point. JMA's seismic intensity scale has 10 degrees (0 (imperceptible), 1, 2, 3, 4, 5 lower, 5 upper, 6 lower, 6 upper, 7). le.html 2016/4/27 FPCJ プレスプレス ブリーフィング 6 JMA
7 Each country has own scale!! JMA seismic intensity scale: Japan 1884-, date: seismic intensity meters 0 to 7, 10 scales (5 and 6 have two scales) Mercalli intensity scale: US, Korea 1902,Mercalli-Cancani-Sieberg intensity (MCS)scale 1931,Mercalli-Wood-Neuman intensity (MWN) scale Now Modified Mercalli intensity scale, MMI scale a scale from I (not felt) to XII (total destruction) Medvedev-Sponheuer-Kárník scale( MSK scale):cis East European countries, Israel, India 1964-, I to XII, 12 scales. China seismic intensity scale(csis):china 1980-, 1999: modified I-XII,12 scales, European macroseismic (EMS)scale: European countries 1988, European Seismological Commission (ESC) 1998, modified to EMS 98 I to XII, 12 scales 2016/4/27 FPCJ プレスプレス ブリーフィング 7
8 Intensities of the 2016 April 14 earthquake Epicenteral Distribution Intensities JMA 8
9 Intensity Distribution of the 2016 April 16 01:25 JMA 9
10 Maximum acceleration at surface Foreshock on April 14 Maximum velocity at surface Mainshock Maximum acceleration at surface Maximum velocity at surface 10
11 GNSS (Global Navigation Satellite System) 20-cm NNE displacement at Jonan station GSI 国土地理院 11
12 97-cm SW displacement at Choyo station GSI 国土地理院 12
13 Long. Lat. Depth length width strike dip rake slip Magnitude GSI 国土地理院 13
14 Coseismic Displacement on the source fault NIED 14
15 Surface displacement (Preliminary) Surface displacement is found along a 10- km-long western part of the Futagawa segment of the Futagawa fault system. The maximum displacement is about 2 m near Do-zon AIST 2016/4/27 FPCJ プレスプレス ブリーフィング 15
16 Location 1 (Tsuchiyama) Right-lateral cm After the April 16 th 01:25 event Location 2(Iida) Vertical displacement of 15 cm 10-cm displacement perpendicular to the fault strace, indicating normal faulting Location 3(Do-zon) Right lateral of about 2 m AIST 16
17 Headquarters for Earthquake Research Promotion (HERP) 17
18 平成 28 年 (2016 年 ) 熊本地震の評価 この震源域付近には日奈久断層帯が存在している 今回の地震は その高野 - 白旗区間の活動によると考えられる 地震調査委員会は日奈久断層帯 ( 高野 - 白旗区間 ) について 活動時に M6.8 程度の地震が発生する可能性があり 30 年以内の地震発生確率は不明と評価していた なお 日奈久断層帯 ( 高野 - 白旗区間 ) を含む九州南部の区域では M6.8 以上の地震の発生確率は 7-18% と評価していた 18
19 平成 28 年 4 月 16 日熊本県熊本地方 の地震の評価 第 289 回 ( 臨時会 ) 平成 28 年 4 月 17 日 この震源域付近には布田川断層帯が存在している 現地調査の結果によると 布田川断層帯の布田川区間沿いなどで地表地震断層が見つかっている この地震は 主に布田川断層帯の布田川区間の活動によると考えられる 地震調査委員会は布田川断層帯 ( 布田川区間 ) について 活動時に M7.0 程度の地震が発生する可能性があり 30 年以内の地震発生確率はほぼ 0%~0.9%( やや高い ) と評価していた なお 布田川断層帯を含む九州中部の区域では M6.8 以上の地震の発生確率は 18-27% と評価していた 19
20 日奈久断層帯 評価区間高野 - 白旗区間断層長約 16 km N23 E 右横ずれ断層南東側隆起を伴う高角度断層面の幅 13 km 程度地震発生層の下限の深さ 13 km 程度平均変位速度 m/ 千年程度 ( 上下 ) 一回のずれ量 2m 程度最新活動時期約 1,600 年前以後 約 1,200 年前以前平均活動間隔 : 不明 20
21 0%~0.9% chance of M7.0 in 30 years Headquarters for Earthquake Research Promotion (HERP) 21
22 Central Kyushu:18-20% Whole Kyushu: 30-42% Headquarters for Earthquake Research Promotion (HERP) 22
23 23 JMA
24 JMA 24
25 JMA 25
26 JMA 2016/4/27 FPCJ プレスプレス ブリーフィング 26
27 As of April 25 13: Kumamoto EQ (M7.3) Niigata-ken Chuetsu EQ (M6.8) 2008 Iwate-Miyagi Inland EQ (M7.2) Kobe EQ (M7.3) 2005 West off Fukuoka EQ (M7.0) 2000 Western Tottori EQ (M7.3) 1997 Satsuma EQ (M6.8) JMA 27
28 Summary On April 14 th and 16 th, 2016, large shallow inland earthquakes occurred in Kumamoto, which generated strong grand motions. April 14the event is M6.5 and 16the is M7.3 Both generated seismic intensity 7 in JMA scale. Those occurred along Futagawa-Hinagu fault system. It was evaluated that a chance of M6.8 or larger in 30 years is 30-42% for a whole Kyushu The 2016 Kumamoto earthquake is associated with prominent foreshock and afterchok activites. 2016/4/27 FPCJ プレスプレス ブリーフィング 28
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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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