{"_buckets": {"deposit": "8596a123-ba11-4154-8a9f-93ff115f2ead"}, "_deposit": {"id": "20460", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "20460"}, "status": "published"}, "_oai": {"id": "oai:soar-ir.repo.nii.ac.jp:00020460", "sets": ["1169:1170"]}, "author_link": ["107410", "107411", "107412", "107413"], "item_1628147817048": {"attribute_name": "\u51fa\u7248\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"subitem_version_resource": "http://purl.org/coar/version/c_970fb48d4fbd8a85", "subitem_version_type": "VoR"}]}, "item_6_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\uff08\u5225\u8a00\u8a9e\u7b49\uff09\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "Submarine canyon-fill slump deposits on the shelf environment of the Pliocene Dainenji Formation on the Pacific coast in Fukushima, northeastern Japan"}]}, "item_6_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2007-04-20", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "105", "bibliographicPageStart": "101", "bibliographicVolumeNumber": "64", "bibliographic_titles": [{"bibliographic_title": "\u5806\u7a4d\u5b66\u7814\u7a76"}]}]}, "item_6_description_20": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "The Dainenji Formation is deposited on shelf environment and consists mainly of sandy siltstone and sandstone. It includes a number of volcanic ash layers, which serve as good key beds useful for precise correlation. Mappable units of submarine canyon-fill sediment are recognized in this area. A valley has a maximum depth of 100 m and is considered to be formed by submarine landslide, which took place after 2.7 Ma. Submarine canyon-fill sediments are composed of siltstone interbedded with thin sandstone layers, thick sandstone beds and slump deposits. 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