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  1. 防災科研関係論文

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/5864
eb0f8051-5430-4008-bf19-2b3559f7c598
Item type researchmap(1)
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

ja 橋本 徹夫

en HASHIMOTO Tetsuo

Search repository
菊地 正幸

× 菊地 正幸

ja 菊地 正幸

en KIKUCHI Masayuki

Search repository
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
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
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