{"created":"2021-03-01T06:23:34.143166+00:00","id":20462,"links":{},"metadata":{"_buckets":{"deposit":"d25afe8b-76a6-44ba-8959-2f70749a7d76"},"_deposit":{"id":"20462","owners":[],"pid":{"revision_id":0,"type":"depid","value":"20462"},"status":"published"},"_oai":{"id":"oai:soar-ir.repo.nii.ac.jp:00020462","sets":["1169:1170"]},"author_link":["107416","107417","107418"],"item_1628147817048":{"attribute_name":"出版タイプ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_6_alternative_title_1":{"attribute_name":"その他（別言語等）のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Tsunami deposits in the estuary-fill:Holocene drill core in Minamisoma City, Fukushima Prefecture, Northeast 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5,500年以降，海退と埋積によりエスチュアリーは縮小し塩水湿地となった．（5）約100年前に干拓により水田となった．さらに，塩水湿地の泥質堆積物に挟在するイベント堆積物は貝化石を含む砂層で，すべて海側から運搬されたと考えられる．また，級化構造，複級化成層，逆級化構造が見られる．さらに，これらのイベント砂層の一部には偽礫や礫が含まれ，斜交ラミナを伴う．砂層の堆積間隔は約600年と見積もられる．以上のことから，これらの砂層の多くは，津波堆積物である可能性が高い．","subitem_description_type":"Abstract"}]},"item_6_description_30":{"attribute_name":"資源タイプ（コンテンツの種類）","attribute_value_mlt":[{"subitem_description":"Article","subitem_description_type":"Other"}]},"item_6_description_5":{"attribute_name":"引用","attribute_value_mlt":[{"subitem_description":"堆積学研究.75(2):73-82(2017)","subitem_description_type":"Other"}]},"item_6_link_3":{"attribute_name":"信州大学研究者総覧へのリンク","attribute_value_mlt":[{"subitem_link_text":"保柳, 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福島県南相馬市小高区井田川地区における完新統ボーリングコア","subitem_title_language":"ja"}]},"item_type_id":"6","owner":"1","path":["1170"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2019-02-22"},"publish_date":"2019-02-22","publish_status":"0","recid":"20462","relation_version_is_last":true,"title":["エスチュアリー埋積堆積物中の津波堆積物 : 福島県南相馬市小高区井田川地区における完新統ボーリングコア"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-14T04:39:14.291767+00:00"}