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{"_buckets": {"deposit": "03115c9d-d096-461a-ba17-f917dd55fcbc"}, "_deposit": {"id": "3114", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "3114"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00003114", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2021-01-01", "bibliographicIssueDateType": "Issued"}, "bibliographicPageStart": "1", "bibliographicVolumeNumber": "73", "bibliographic_titles": [{"bibliographic_title": "Earth, Planets and Space", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "\u003ctitle\u003eAbstract\u003c/title\u003eThe tectonic stress field was investigated in and around the aftershock area of the Hokkaido Eastern Iburi earthquake (\u003citalic\u003eM\u003c/italic\u003e\u003csub\u003eJMA\u003c/sub\u003e?=?6.7) occurred on 6 September 2018. We deployed 26 temporary seismic stations in the aftershock area for approximately 2?months and located 1785 aftershocks precisely. Among these aftershocks, 894 focal mechanism solutions were determined using the first-motion polarity of P wave from the temporary observation and the permanent seismic networks of Hokkaido University, Japan Meteorological Agency (JMA), and High Sensitivity Seismograph Network Japan (Hi-net). We found that (1) the reverse faulting and the strike-slip faulting are dominant in the aftershock area, (2) the average trend of P- and T-axes is 78°?±?33° and 352°?±?51°, respectively, and (3) the average plunge of P- and T-axes is 25°?±?16° and 44°?±?20°, respectively: the P-axis is close to be horizontal and the T-axis is more vertical than the average of the P-axes. We applied a stress inversion method to the focal mechanism solutions to estimate a stress field in the aftershock area. As a result, we found that the reverse fault type stress field is dominant in the aftershock area. An axis of the maximum principal stress (\u003citalic\u003eσ\u003c/italic\u003e\u003csub\u003e1\u003c/sub\u003e) has the trend of 72°?±?7° and the dipping eastward of 19°?±?4° and an axis of the intermediate principal stress (\u003citalic\u003eσ\u003c/italic\u003e\u003csub\u003e2\u003c/sub\u003e) has the trend of 131°?±?73° and the dipping southward of 10°?±?9°, indicating that both of \u003citalic\u003eσ\u003c/italic\u003e\u003csub\u003e1\u003c/sub\u003e- and \u003citalic\u003eσ\u003c/italic\u003e\u003csub\u003e2\u003c/sub\u003e-axes are close to be horizontal. An axis of the minimum principal stress (\u003citalic\u003eσ\u003c/italic\u003e\u003csub\u003e3\u003c/sub\u003e) has the dipping westward of 67°?±?6° that is close to be vertical. The results strongly suggest that the reverse-fault-type stress field is predominant as an average over the aftershock area which is in the western boundary of the Hidaka Collision Zone. The average of the stress ratio \u003citalic\u003eR\u003c/italic\u003e?=?(\u003citalic\u003eσ\u003c/italic\u003e\u003csub\u003e1\u003c/sub\u003e???\u003citalic\u003eσ\u003c/italic\u003e\u003csub\u003e2\u003c/sub\u003e)/(\u003citalic\u003eσ\u003c/italic\u003e\u003csub\u003e1\u003c/sub\u003e???\u003citalic\u003eσ\u003c/italic\u003e\u003csub\u003e3\u003c/sub\u003e) is 0.61?±?0.13 in the whole aftershock area. Although not statistically significant, we suggest that \u003citalic\u003eR\u003c/italic\u003e decreases systematically as the depth is getting deep, which is modeled by a quadratic polynomial of depth.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "Springer Science and Business Media LLC", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1186/s40623-020-01323-x"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "1880-5981", "subitem_source_identifier_type": "EISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Yuki Susukida", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Kei Katsumata", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Masayoshi Ichiyanagi", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Mako Ohzono", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Hiroshi Aoyama", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Ryo Tanaka", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Masamitsu Takada", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Teruhiro Yamaguchi", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Kazumi Okada", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Hiroaki Takahashi", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Shin’ichi Sakai", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Satoshi Matsumoto", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Tomomi Okada", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Toru Matsuzawa", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Hiroki Miyamachi", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Shuichiro Hirano", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Yoshiko Yamanaka", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Shinichiro Horikawa", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Masahiro Kosuga", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Hiroshi Katao", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Yoshihisa Iio", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Airi Nagaoka", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Noriko Tsumura", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Tomotake Ueno", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Focal mechanisms and the stress field in the aftershock area of the 2018 Hokkaido Eastern Iburi earthquake (MJMA?=?6.7)", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Focal mechanisms and the stress field in the aftershock area of the 2018 Hokkaido Eastern Iburi earthquake (MJMA?=?6.7)", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/3114", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "3114", "relation": {}, "relation_version_is_last": true, "title": ["Focal mechanisms and the stress field in the aftershock area of the 2018 Hokkaido Eastern Iburi earthquake (MJMA?=?6.7)"], "weko_shared_id": -1}
  1. 防災科研関係論文

Focal mechanisms and the stress field in the aftershock area of the 2018 Hokkaido Eastern Iburi earthquake (MJMA?=?6.7)

https://nied-repo.bosai.go.jp/records/3114
https://nied-repo.bosai.go.jp/records/3114
89c042a7-0253-4e67-8c04-1795a2f386b8
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Focal mechanisms and the stress field in the aftershock area of the 2018 Hokkaido Eastern Iburi earthquake (MJMA?=?6.7)
言語
言語 eng
著者 Yuki Susukida

× Yuki Susukida

en Yuki Susukida

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Kei Katsumata

× Kei Katsumata

en Kei Katsumata

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Masayoshi Ichiyanagi

× Masayoshi Ichiyanagi

en Masayoshi Ichiyanagi

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Mako Ohzono

× Mako Ohzono

en Mako Ohzono

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Hiroshi Aoyama

× Hiroshi Aoyama

en Hiroshi Aoyama

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Ryo Tanaka

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en Ryo Tanaka

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Masamitsu Takada

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en Masamitsu Takada

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Teruhiro Yamaguchi

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en Teruhiro Yamaguchi

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Kazumi Okada

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en Kazumi Okada

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Hiroaki Takahashi

× Hiroaki Takahashi

en Hiroaki Takahashi

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Shin’ichi Sakai

× Shin’ichi Sakai

en Shin’ichi Sakai

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Satoshi Matsumoto

× Satoshi Matsumoto

en Satoshi Matsumoto

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Tomomi Okada

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en Tomomi Okada

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Toru Matsuzawa

× Toru Matsuzawa

en Toru Matsuzawa

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Hiroki Miyamachi

× Hiroki Miyamachi

en Hiroki Miyamachi

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Shuichiro Hirano

× Shuichiro Hirano

en Shuichiro Hirano

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Yoshiko Yamanaka

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en Yoshiko Yamanaka

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Shinichiro Horikawa

× Shinichiro Horikawa

en Shinichiro Horikawa

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Masahiro Kosuga

× Masahiro Kosuga

en Masahiro Kosuga

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Hiroshi Katao

× Hiroshi Katao

en Hiroshi Katao

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Yoshihisa Iio

× Yoshihisa Iio

en Yoshihisa Iio

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Airi Nagaoka

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en Airi Nagaoka

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Noriko Tsumura

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Tomotake Ueno

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抄録
内容記述タイプ Other
内容記述 <title>Abstract</title>The tectonic stress field was investigated in and around the aftershock area of the Hokkaido Eastern Iburi earthquake (<italic>M</italic><sub>JMA</sub>?=?6.7) occurred on 6 September 2018. We deployed 26 temporary seismic stations in the aftershock area for approximately 2?months and located 1785 aftershocks precisely. Among these aftershocks, 894 focal mechanism solutions were determined using the first-motion polarity of P wave from the temporary observation and the permanent seismic networks of Hokkaido University, Japan Meteorological Agency (JMA), and High Sensitivity Seismograph Network Japan (Hi-net). We found that (1) the reverse faulting and the strike-slip faulting are dominant in the aftershock area, (2) the average trend of P- and T-axes is 78°?±?33° and 352°?±?51°, respectively, and (3) the average plunge of P- and T-axes is 25°?±?16° and 44°?±?20°, respectively: the P-axis is close to be horizontal and the T-axis is more vertical than the average of the P-axes. We applied a stress inversion method to the focal mechanism solutions to estimate a stress field in the aftershock area. As a result, we found that the reverse fault type stress field is dominant in the aftershock area. An axis of the maximum principal stress (<italic>σ</italic><sub>1</sub>) has the trend of 72°?±?7° and the dipping eastward of 19°?±?4° and an axis of the intermediate principal stress (<italic>σ</italic><sub>2</sub>) has the trend of 131°?±?73° and the dipping southward of 10°?±?9°, indicating that both of <italic>σ</italic><sub>1</sub>- and <italic>σ</italic><sub>2</sub>-axes are close to be horizontal. An axis of the minimum principal stress (<italic>σ</italic><sub>3</sub>) has the dipping westward of 67°?±?6° that is close to be vertical. The results strongly suggest that the reverse-fault-type stress field is predominant as an average over the aftershock area which is in the western boundary of the Hidaka Collision Zone. The average of the stress ratio <italic>R</italic>?=?(<italic>σ</italic><sub>1</sub>???<italic>σ</italic><sub>2</sub>)/(<italic>σ</italic><sub>1</sub>???<italic>σ</italic><sub>3</sub>) is 0.61?±?0.13 in the whole aftershock area. Although not statistically significant, we suggest that <italic>R</italic> decreases systematically as the depth is getting deep, which is modeled by a quadratic polynomial of depth.
言語 en
書誌情報 en : Earth, Planets and Space

巻 73, p. 1, 発行日 2021-01-01
出版者
言語 en
出版者 Springer Science and Business Media LLC
ISSN
収録物識別子タイプ EISSN
収録物識別子 1880-5981
DOI
関連識別子 10.1186/s40623-020-01323-x
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