{"_buckets": {"deposit": "d4a9ca34-4f1d-4d5b-bf68-ff0977f2d8e1"}, "_deposit": {"id": "5846", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "5846"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00005846", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1991", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "3", "bibliographicPageEnd": "201", "bibliographicPageStart": "185", "bibliographicVolumeNumber": "44", "bibliographic_titles": [{"bibliographic_title": "地震 第2輯", "bibliographic_titleLang": "ja"}, {"bibliographic_title": "Zisin (Journal of the Seismological Society of Japan. 2nd ser.)", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "We derived three-dimensional P-wave velocity structure beneath the Japanese Islands by a tomographic inversion of travel time data. We used 37, 617 arrival time data from 581 earthquakes observed at 99 Japan Meteorological Agency stations by high-sensitive type seismometers (EMT, EMT76 and OBS) and estimated the velocity anomalies in a number of blocks and corrections to the source parameters simultaneously. In this study we used a block size of 0.5\u0026deg;\u0026times;0.\u0026deg;\u0026times;50km (for the uppermost three layers, 0.5\u0026deg;\u0026times;0.5\u0026deg;\u0026times;33km).\u003cbr\u003eDown to a depth of about 300km, we obtained detailed features. High velocity anomalies corresponding to the Pacific slab from Hokkaido to Kanto district and the Philippine Sea slab from Aichi prefecture to Shikoku are well delineated. Especially, we found aseismic extension of the Philippine Sea slab beneath the Japan Sea coast of Chugoku district. Low velocity anomalies corresponding to the volcanic front and the wedge portion of the upper mantle are found. We also see low velocity anomalies on the oceanic side of the Pacific slab below the depth of 250km.\u003cbr\u003eIn comparison with the result from ISC data obtained by Kamiya \u003ci\u003eet al.\u003c/i\u003e in 1989, we got clearer images in this study in the shallow regions down to a depth of about 300km, because of accurate data used in this study. The efficiency of this data set for travel time inversions like as this study is found to be comparable to the Japan University Network Earthquake Catalog data.", "subitem_description_language": "ja", "subitem_description_type": "Other"}, {"subitem_description": "We derived three-dimensional P-wave velocity structure beneath the Japanese Islands by a tomographic inversion of travel time data. We used 37, 617 arrival time data from 581 earthquakes observed at 99 Japan Meteorological Agency stations by high-sensitive type seismometers (EMT, EMT76 and OBS) and estimated the velocity anomalies in a number of blocks and corrections to the source parameters simultaneously. In this study we used a block size of 0.5\u0026deg;\u0026times;0.\u0026deg;\u0026times;50km (for the uppermost three layers, 0.5\u0026deg;\u0026times;0.5\u0026deg;\u0026times;33km).\u003cbr\u003eDown to a depth of about 300km, we obtained detailed features. High velocity anomalies corresponding to the Pacific slab from Hokkaido to Kanto district and the Philippine Sea slab from Aichi prefecture to Shikoku are well delineated. Especially, we found aseismic extension of the Philippine Sea slab beneath the Japan Sea coast of Chugoku district. Low velocity anomalies corresponding to the volcanic front and the wedge portion of the upper mantle are found. We also see low velocity anomalies on the oceanic side of the Pacific slab below the depth of 250km.\u003cbr\u003eIn comparison with the result from ISC data obtained by Kamiya \u003ci\u003eet al.\u003c/i\u003e in 1989, we got clearer images in this study in the shallow regions down to a depth of about 300km, because of accurate data used in this study. The efficiency of this data set for travel time inversions like as this study is found to be comparable to the Japan University Network Earthquake Catalog data.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "公益社団法人 日本地震学会", "subitem_publisher_language": "ja"}, {"subitem_publisher": "SEISMOLOGICAL SOCIETY OF JAPAN", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.4294/zisin1948.44.3_185"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0037-1114", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "神谷 眞一郎", "creatorNameLang": "ja"}, {"creatorName": "KAMIYA Shin\u0027ichiro", "creatorNameLang": "en"}]}]}, "item_title": "気象庁地震月報データから求めた日本列島下の3次元地震波速度構造", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "気象庁地震月報データから求めた日本列島下の3次元地震波速度構造", "subitem_title_language": "ja"}, {"subitem_title": "Three-dimensional P-wave Velocity Structure beneath the Japanese Islands Estimated from the Seismological Bulletin of the Japan Meteorological Agency", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/5846", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "5846", "relation": {}, "relation_version_is_last": true, "title": ["気象庁地震月報データから求めた日本列島下の3次元地震波速度構造"], "weko_shared_id": -1}