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{"_buckets": {"deposit": "a6b7d528-2b81-4490-aa47-ca4c6d7046f4"}, "_deposit": {"id": "5825", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "5825"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00005825", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1990", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "5", "bibliographicPageEnd": "360", "bibliographicPageStart": "347", "bibliographicVolumeNumber": "38", "bibliographic_titles": [{"bibliographic_title": "Journal of Physics of the Earth", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "In October-November, 1989, five M?6 earthquakes, including an M7.1 earthquake, sequentially took place off Sanriku, northeastern Japan, and the earthquake activity became very high in this region. Since the seismically active zone was far from the land observation network, it was difficult to obtain accurate hypocenter locations. We carried out ocean bottom seismographic observation in order to locate the hypocenters precisely and investigate characteristics of the activity. Combining the OBS and land station data for hypocenter determination, we obtained two main conclusions. (1) Almost all epicenters of the present activity distribute landward from the 4 km isobath. Some earthquake clusters were observed including an M5.6 earthquake and its aftershocks. (2) Focal depths of the earthquakes are shallower than 20 km and the activity is interpreted to take place around the boundary between the subducting Pacific plate and the landward plate. Taking account of the mechanisms of the larger earthquakes in this active period, this activity is a thrust fault type and is different from the 1933 Sanriku earthquake which was a normal fault type and might have broken the entire oceanic lithosphere. c 1990, The Seismological Society of Japan, The Volcanological Society of Japan, The Geodetic Society of Japan. All rights reserved.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.4294/jpe1952.38.347"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0022-3743", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Azusa Nishizawa", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Toshio Kono", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Akira Hasegawa", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Tomowo Hirasawa", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Toshihiko Kanazawa", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Takaya Iwasaki", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Spatial Distribution of Earthquakes off Sanriku, Northeastern Japan, in 1989 Determined by Ocean-Bottom and Land-Based Observation", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Spatial Distribution of Earthquakes off Sanriku, Northeastern Japan, in 1989 Determined by Ocean-Bottom and Land-Based Observation", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/5825", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "5825", "relation": {}, "relation_version_is_last": true, "title": ["Spatial Distribution of Earthquakes off Sanriku, Northeastern Japan, in 1989 Determined by Ocean-Bottom and Land-Based Observation"], "weko_shared_id": -1}
  1. 防災科研関係論文

Spatial Distribution of Earthquakes off Sanriku, Northeastern Japan, in 1989 Determined by Ocean-Bottom and Land-Based Observation

https://nied-repo.bosai.go.jp/records/5825
https://nied-repo.bosai.go.jp/records/5825
3e261d84-2dd8-4d80-bea0-503ec8beefaa
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Spatial Distribution of Earthquakes off Sanriku, Northeastern Japan, in 1989 Determined by Ocean-Bottom and Land-Based Observation
言語
言語 eng
著者 Azusa Nishizawa

× Azusa Nishizawa

en Azusa Nishizawa

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Toshio Kono

× Toshio Kono

en Toshio Kono

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Akira Hasegawa

× Akira Hasegawa

en Akira Hasegawa

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Tomowo Hirasawa

× Tomowo Hirasawa

en Tomowo Hirasawa

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Toshihiko Kanazawa

× Toshihiko Kanazawa

en Toshihiko Kanazawa

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Takaya Iwasaki

× Takaya Iwasaki

en Takaya Iwasaki

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抄録
内容記述タイプ Other
内容記述 In October-November, 1989, five M?6 earthquakes, including an M7.1 earthquake, sequentially took place off Sanriku, northeastern Japan, and the earthquake activity became very high in this region. Since the seismically active zone was far from the land observation network, it was difficult to obtain accurate hypocenter locations. We carried out ocean bottom seismographic observation in order to locate the hypocenters precisely and investigate characteristics of the activity. Combining the OBS and land station data for hypocenter determination, we obtained two main conclusions. (1) Almost all epicenters of the present activity distribute landward from the 4 km isobath. Some earthquake clusters were observed including an M5.6 earthquake and its aftershocks. (2) Focal depths of the earthquakes are shallower than 20 km and the activity is interpreted to take place around the boundary between the subducting Pacific plate and the landward plate. Taking account of the mechanisms of the larger earthquakes in this active period, this activity is a thrust fault type and is different from the 1933 Sanriku earthquake which was a normal fault type and might have broken the entire oceanic lithosphere. c 1990, The Seismological Society of Japan, The Volcanological Society of Japan, The Geodetic Society of Japan. All rights reserved.
言語 en
書誌情報 en : Journal of Physics of the Earth

巻 38, 号 5, p. 347-360, 発行日 1990
ISSN
収録物識別子タイプ ISSN
収録物識別子 0022-3743
DOI
関連識別子 10.4294/jpe1952.38.347
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