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地震記象から見た1946年南海地震の震源過程
https://nied-repo.bosai.go.jp/records/5864
https://nied-repo.bosai.go.jp/records/5864eb0f8051-5430-4008-bf19-2b3559f7c598
Item type | researchmap(1) | |||||||||||||
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公開日 | 2023-03-30 | |||||||||||||
タイトル | ||||||||||||||
言語 | ja | |||||||||||||
タイトル | 地震記象から見た1946年南海地震の震源過程 | |||||||||||||
タイトル | ||||||||||||||
言語 | en | |||||||||||||
タイトル | Source Process of the 1946 Nankai Earthquake Estimated from Seismograms | |||||||||||||
言語 | ||||||||||||||
言語 | jpn | |||||||||||||
著者 |
橋本 徹夫
× 橋本 徹夫
× 菊地 正幸
|
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抄録 | ||||||||||||||
内容記述タイプ | Other | |||||||||||||
内容記述 | Subevents of the 1946 Nankai earthquake (<I>M</I><SUB>jma</SUB>8.0) were distinguished from seismograms recorded on smoked papers with strong motion seismograms (T<SUB>0</SUB>=6s, amplification=2) and seismological data of Japan Meteorological Agency. Location and origin time of each subevent were roughly estimated from a hypocenter determination with phase readings of P and S waves for the subevent. Rupture of the Nankai earthquake started at a point southward about 50km off Cape Shionomisaki (first subevent). The rupture propagated in the NNW direction with a rupture velocity of 1.9 km/s and a second subevent that grew to class <I>M</I>8 started after about 16 sec from the initiation of the first subevent. Then the rupture propagated westward, and third subevent of <I>M</I>8 occurred around Tosa Bay, located about 200 km from the second event, about 53 sec after the initiation of the second event. Seismic waves were excited near Tosa Bay during the 1946 Nankai earthquake. | |||||||||||||
言語 | ja | |||||||||||||
抄録 | ||||||||||||||
内容記述タイプ | Other | |||||||||||||
内容記述 | Subevents of the 1946 Nankai earthquake (<I>M</I><SUB>jma</SUB>8.0) were distinguished from seismograms recorded on smoked papers with strong motion seismograms (T<SUB>0</SUB>=6s, amplification=2) and seismological data of Japan Meteorological Agency. Location and origin time of each subevent were roughly estimated from a hypocenter determination with phase readings of P and S waves for the subevent. Rupture of the Nankai earthquake started at a point southward about 50km off Cape Shionomisaki (first subevent). The rupture propagated in the NNW direction with a rupture velocity of 1.9 km/s and a second subevent that grew to class <I>M</I>8 started after about 16 sec from the initiation of the first subevent. Then the rupture propagated westward, and third subevent of <I>M</I>8 occurred around Tosa Bay, located about 200 km from the second event, about 53 sec after the initiation of the second event. Seismic waves were excited near Tosa Bay during the 1946 Nankai earthquake. | |||||||||||||
言語 | en | |||||||||||||
書誌情報 |
ja : 地學雜誌 en : Journal of Geography (Chigaku Zasshi) 巻 111, 号 1, p. 118-125, 発行日 2002-02-25 |
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出版者 | ||||||||||||||
言語 | ja | |||||||||||||
出版者 | 公益社団法人 東京地学協会 | |||||||||||||
出版者 | ||||||||||||||
言語 | en | |||||||||||||
出版者 | Tokyo Geographical Society | |||||||||||||
ISSN | ||||||||||||||
収録物識別子タイプ | ISSN | |||||||||||||
収録物識別子 | 0022-135X | |||||||||||||
DOI | ||||||||||||||
関連識別子 | 10.5026/jgeography.111.118 |