{"_buckets": {"deposit": "21e8a48a-b610-46c2-9708-900629615b2f"}, "_deposit": {"id": "4447", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "4447"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00004447", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2000-07"}, "bibliographicIssueNumber": "13", "bibliographicPageEnd": "1948", "bibliographicPageStart": "1945", "bibliographicVolumeNumber": "27", "bibliographic_titles": [{"bibliographic_title": "GEOPHYSICAL RESEARCH LETTERS", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "We have obtained a snapshot image of the earthquake activity along the northern Reykjanes Ridge (RR) using a dense ocean bottom seismometer (OBS) array. The earthquakes are narrowly concentrated along the NE-SW trending ridge crest. The seismicity is segmented into clusters by the en-echelon NNE-SSW trending axial volcanic systems which characterize the obliquely spreading ridge. The hypocenters are concentrated at somewhat greater depths (3-7 km) than on the Reykjanes Peninsula (RP), where the crust is thicker. Normal faulting dominates at the ridge crest. The focal planes are oriented more NE-SW than NNE-SSW, i.e., parallel to the ridge crest and its peripheral faults rather than the trend of individual axial volcanic systems and associated faults.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "AMER GEOPHYSICAL UNION", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1029/1999GL011264"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0094-8276", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "M Mochizuki", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "B Brandsdottir", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "H Shiobara", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "G Gudmundsson", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "R Stefansson", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "H Shimamura", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Detailed distribution of microearthquakes along the northern Reykjanes Ridge, off SW-Iceland", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Detailed distribution of microearthquakes along the northern Reykjanes Ridge, off SW-Iceland", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/4447", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "4447", "relation": {}, "relation_version_is_last": true, "title": ["Detailed distribution of microearthquakes along the northern Reykjanes Ridge, off SW-Iceland"], "weko_shared_id": -1}