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  1. 防災科研関係論文

Sediment deformation in eastern Sagami Bay revealed by high-density seismic reflection survey

https://nied-repo.bosai.go.jp/records/4001
https://nied-repo.bosai.go.jp/records/4001
149c1bf4-d1b3-4afb-84c1-0cdcd5aa7e2b
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 ja
タイトル Sediment deformation in eastern Sagami Bay revealed by high-density seismic reflection survey
タイトル
言語 en
タイトル Sediment deformation in eastern Sagami Bay revealed by high-density seismic reflection survey
言語
言語 eng
著者 Yamashita Mikiya

× Yamashita Mikiya

ja Yamashita Mikiya

en Yamashita Mikiya

Search repository
Kinoshita Masataka

× Kinoshita Masataka

ja Kinoshita Masataka

en Kinoshita Masataka

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Kasaya Takafumi

× Kasaya Takafumi

ja Kasaya Takafumi

en Kasaya Takafumi

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Takahashi Narumi

× Takahashi Narumi

ja Takahashi Narumi

en Takahashi Narumi

Search repository
Kaneda Yoshiyuki

× Kaneda Yoshiyuki

ja Kaneda Yoshiyuki

en Kaneda Yoshiyuki

Search repository
抄録
内容記述タイプ Other
内容記述 Sagami Bay is known as a seismogenic area occurring large earthquakes repeatedly with M > 7 at the boundary between the Philippine Sea plate and the overriding northeastern Japan with the Quaternary sediments. To investigate this area for understanding the mechanism of repeated large earthquakes, we carried out a high density single-channel seismic reflection survey around Sagami Bay in April - May, 2005 using R/V <i>Kaiyo</i> of Japan Agency for Marine-Earth Science and Technology (JAMSTEC). We propose new growth scenario of a unique reverse fault associated with the 1923 Kanto earthquake in the Sagami Trough in this paper as follows from units of sedimentary layers of the seismic profiles provided tectonics information studies of the clear sedimentary facies is indicated along the Sagami Trough. In particular, the fault with reverse sense displacement of ENE-WSW strike is recognized in the Sunosaki Canyon. This reverse fault is located on the asperity of the large aftershock epicenter (M7.3) in the 1923 Kanto earthquake. There is no active fault in the seafloor of sedimentary layers from this reverse sense displacement to onshore. Thus, this displacement would be developed with the subducting Philippine Sea plate. We propose the growth process of obtained reverse sense displacement in Sagami Trough.
言語 ja
抄録
内容記述タイプ Other
内容記述 Sagami Bay is known as a seismogenic area occurring large earthquakes repeatedly with M > 7 at the boundary between the Philippine Sea plate and the overriding northeastern Japan with the Quaternary sediments. To investigate this area for understanding the mechanism of repeated large earthquakes, we carried out a high density single-channel seismic reflection survey around Sagami Bay in April - May, 2005 using R/V <i>Kaiyo</i> of Japan Agency for Marine-Earth Science and Technology (JAMSTEC). We propose new growth scenario of a unique reverse fault associated with the 1923 Kanto earthquake in the Sagami Trough in this paper as follows from units of sedimentary layers of the seismic profiles provided tectonics information studies of the clear sedimentary facies is indicated along the Sagami Trough. In particular, the fault with reverse sense displacement of ENE-WSW strike is recognized in the Sunosaki Canyon. This reverse fault is located on the asperity of the large aftershock epicenter (M7.3) in the 1923 Kanto earthquake. There is no active fault in the seafloor of sedimentary layers from this reverse sense displacement to onshore. Thus, this displacement would be developed with the subducting Philippine Sea plate. We propose the growth process of obtained reverse sense displacement in Sagami Trough.
言語 en
書誌情報 ja : JAMSTEC Report of Research and Development
en : JAMSTEC Rep. Res. Dev.

巻 17, p. 1-10
出版者
言語 ja
出版者 Japan Agency for Marine-Earth Science and Technology
出版者
言語 en
出版者 Japan Agency for Marine-Earth Science and Technology
ISSN
収録物識別子タイプ ISSN
収録物識別子 1880-1153
DOI
関連識別子 10.5918/jamstecr.17.1
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