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  1. 防災科研関係論文

A new method for determining OBS positions for crustal structure studies, using airgun shots and precise bathymetric data

https://nied-repo.bosai.go.jp/records/4654
https://nied-repo.bosai.go.jp/records/4654
5f6f7d86-3454-4936-8b96-1c9df3e14271
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル A new method for determining OBS positions for crustal structure studies, using airgun shots and precise bathymetric data
言語
言語 eng
著者 Atsushi Oshida

× Atsushi Oshida

en Atsushi Oshida

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Ryuji Kubota

× Ryuji Kubota

en Ryuji Kubota

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Eiichiro Nishiyama

× Eiichiro Nishiyama

en Eiichiro Nishiyama

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Jun Ando

× Jun Ando

en Jun Ando

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Junzo Kasahara

× Junzo Kasahara

en Junzo Kasahara

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Azusa Nishizawa

× Azusa Nishizawa

en Azusa Nishizawa

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Kentaro Kaneda

× Kentaro Kaneda

en Kentaro Kaneda

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抄録
内容記述タイプ Other
内容記述 Ocean-bottom seismometer (OBS) positions are one of the key parameters in an OBS-airgun seismic survey for crustal structure study. To improve the quality of these parameters, we have developed a new method of determining OBS positions, using airgun shot data and bathymetric data in addition to available distance measurements by acoustic transponders. The traveltimes of direct water waves emitted by airgun shots and recorded by OBSs are used as important information for determining OBS locations, in cases where there are few acoustic transponder data (&lt
3 sites). The new method consists of two steps. A global search is performed as the first step, to find nodes of the bathymetric grid that are the closest to explaining the observed direct water-wave traveltimes from airgun shots, and acoustic ranging using a transponder system. The use of precise 2D bathymetric data is most important if the bottom topography near the OBS is extremely rough. The locations of the nodes obtained by the first step are used as initial values for the second step, to avoid falling into local convergence minima. In the second step, a non-linear inverse method is executed. If the OBS internal clock shows large drift, a secondary correction for the OBS internal clock is obtained, as well as the OBS location, as final results by this method. We discuss the error and the influence of each measurement used in the determination of OBS location. c ASEG/SEGJ/KSEG 2008.
言語 en
書誌情報 en : Exploration Geophysics

巻 39, 号 1, p. 15-25, 発行日 2008
ISSN
収録物識別子タイプ ISSN
収録物識別子 0812-3985
DOI
関連識別子 10.1071/EG08005
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