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  1. 防災科研関係論文

Seafloor borehole broadband seismic observatories in the western pacific and performance of recovered seismic data

https://nied-repo.bosai.go.jp/records/2960
https://nied-repo.bosai.go.jp/records/2960
79e57a67-1288-4901-a81b-df93b66dee15
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Seafloor borehole broadband seismic observatories in the western pacific and performance of recovered seismic data
著者 Masanao Shinohara

× Masanao Shinohara

en Masanao Shinohara

Search repository
Ei'ichiro Araki

× Ei'ichiro Araki

en Ei'ichiro Araki

Search repository
Toshihiko Kanazawa

× Toshihiko Kanazawa

en Toshihiko Kanazawa

Search repository
Kiyoshi Suyehiro

× Kiyoshi Suyehiro

en Kiyoshi Suyehiro

Search repository
Masashi Mochizuki

× Masashi Mochizuki

en Masashi Mochizuki

Search repository
Tomoaki Yamada

× Tomoaki Yamada

en Tomoaki Yamada

Search repository
Kimihiro Mochizuki

× Kimihiro Mochizuki

en Kimihiro Mochizuki

Search repository
Kazuo Nakahigashi

× Kazuo Nakahigashi

en Kazuo Nakahigashi

Search repository
Yuka Kaiho

× Yuka Kaiho

en Yuka Kaiho

Search repository
抄録
内容記述タイプ Other
内容記述 In 2000 and 2001, the seafloor borehole seismological observatories WP-1 and WP-2 in the northwestern Pacific were installed. The WP-1 site is in the west Philippine Basin, and the WP-2 observatory is situated on a normal oceanic Mesozoic crust in the northwestern Pacific Basin. The WP-1 observatory was activated in March 2002 using the ROV KAIKO and long-term observation was started. In June 2006, the new ROV KAIKO-7000II dived to the WP-1 (fourth visit) and recovered the data. At present, seismic records of 692-days (Mar. 2002 - Feb. 2004) have been obtained from the WP-1. The WP-2 observatory was activated in October 2000 using the KAIKO. In June 2005, the KAIKO-7000 made fourth visit to the WP-2 and recovered the data. Recording at the WP-2 has been suspended from the fourth ROV visit. In total, 436-days data (Oct. 2000 - Jan. 2001, Aug. 2001 - July 2002) were retrieved. The long-term variations of broadband seismic noise spectra (3mHz - 10 Hz) in oceanic basins were revealed. The stable ambient seismic noise levels enable us to record many teleseismic events uniformly in time. Especially, events with magnitudes greater than 6.5 were clearly recorded with a good signal to noise ratio. c 2007 IEEE.
言語 en
書誌情報 en : International Symposium on Underwater Technology, UT 2007 - International Workshop on Scientific Use of Submarine Cables and Related Technologies 2007

p. 682-690, 発行日 2007
DOI
関連識別子 10.1109/UT.2007.370821
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