{"_buckets": {"deposit": "26ee6f6f-67b0-499e-b053-19bcadf3addf"}, "_deposit": {"id": "5831", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "5831"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00005831", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1996", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "5", "bibliographicPageEnd": "552", "bibliographicPageStart": "543", "bibliographicVolumeNumber": "44", "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": "We estimated the basement depth in Kobe City from array records of aftershocks of the 1995 Hyogo-ken Nanbu earthquake. The array measurements were conducted along the Sumiyoshi River in Kobe City using 12 stations from north to south within a distance of about 2 km. Travel time analyses of initial P- and S-waves were made to obtain travel time residuals due to the sediments. We also obtained the travel time difference between S-wave and SP-wave (i.e., P-wave converted from S-wave) at the basement-sediment boundary. By compiling three travel time data sets, we estimated the distribution of the basement depth. The basement depth suddenly increases from 0 to 1 km within a distance of 1 km, and then the depth gently increases to the south.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "CENTER ACADEMIC PUBL 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/jpe1952.44.543"}}]}, "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": "H Yamanaka", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "S Aoi", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Estimation of basement depth along the Sumiyoshi River in Kobe city - Travel time analysis of P-, S-, and SP-waves from an earthquake array observation", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Estimation of basement depth along the Sumiyoshi River in Kobe city - Travel time analysis of P-, S-, and SP-waves from an earthquake array observation", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/5831", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "5831", "relation": {}, "relation_version_is_last": true, "title": ["Estimation of basement depth along the Sumiyoshi River in Kobe city - Travel time analysis of P-, S-, and SP-waves from an earthquake array observation"], "weko_shared_id": -1}