{"created":"2023-06-20T14:52:26.411527+00:00","id":20579,"links":{},"metadata":{"_buckets":{"deposit":"90b51cca-9f5b-4628-bb86-0523574c7cb5"},"_deposit":{"created_by":1,"id":"20579","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"20579"},"status":"published"},"_oai":{"id":"oai:jaxa.repo.nii.ac.jp:00020579","sets":["1543:1778:1792","1887:1891"]},"author_link":["196344","196346","196347","196348","196345","196343"],"item_5_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"クレーター形成速度における先端部と尾部の非対称性の結果として月の地殻2分と再方位"}]},"item_5_biblio_info_10":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2004-02","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"4","bibliographicPageStart":"1","bibliographic_titles":[{"bibliographic_title":"第37回月・惑星シンポジウム"},{"bibliographic_title":"Proceedings of the 37th ISAS Lunar and Planetary Symposium","bibliographic_titleLang":"en"}]}]},"item_5_description_17":{"attribute_name":"抄録（英）","attribute_value_mlt":[{"subitem_description":"Impacts on the early Moon are expected to have been extremely asymmetrical between the leading and trailing hemispheres because of a fast orbital motion of the Moon. In this paper, suggested is an influence of the heavy asymmetrical bombardment upon the rotational dynamics of the early Moon. The preferential bombardment thinned the crust of the leading hemisphere and thickened that of the trailing hemisphere. As a consequence of the redistribution of crustal materials, the axis of the minimum principal moment of inertia shifted toward the west. The Moon was reoriented eastwards with the new minimum axis along the Earth-Moon line. The sequential actions operated continuously and concurrently on the early Moon, so that the Moon was gradually rotated toward the east. Longitudinal distributions of impact basins and crustal thickness models support the scenario proposed here.","subitem_description_type":"Other"}]},"item_5_description_32":{"attribute_name":"資料番号","attribute_value_mlt":[{"subitem_description":"資料番号: AA0047898001","subitem_description_type":"Other"}]},"item_5_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"宇宙航空研究開発機構宇宙科学研究本部"}]},"item_5_publisher_9":{"attribute_name":"出版者（英）","attribute_value_mlt":[{"subitem_publisher":"Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency (JAXA/ISAS)"}]},"item_5_text_6":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"金沢大学 大学院自然科学研究科"},{"subitem_text_value":"金沢大学 大学院自然科学研究科"},{"subitem_text_value":"金沢大学 大学院自然科学研究科"}]},"item_5_text_7":{"attribute_name":"著者所属（英）","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Kanazawa University Graduate School of Natural Science and Technology"},{"subitem_text_language":"en","subitem_text_value":"Kanazawa University Graduate School of Natural Science and Technology"},{"subitem_text_language":"en","subitem_text_value":"Kanazawa University Graduate School of Natural Science and Technology"}]},"item_access_right":{"attribute_name":"アクセス権","attribute_value_mlt":[{"subitem_access_right":"metadata only access","subitem_access_right_uri":"http://purl.org/coar/access_right/c_14cb"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"諸田, 智克"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"鵜飼, 啓之"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"古本, 宗充"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Morota, Tomokatsu","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Ukai, Takashi","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Furumoto, Muneyoshi","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"月","subitem_subject_scheme":"Other"},{"subitem_subject":"地殻2分","subitem_subject_scheme":"Other"},{"subitem_subject":"回転動力学","subitem_subject_scheme":"Other"},{"subitem_subject":"慣性モーメント","subitem_subject_scheme":"Other"},{"subitem_subject":"構造的水盤","subitem_subject_scheme":"Other"},{"subitem_subject":"月地殻厚さ","subitem_subject_scheme":"Other"},{"subitem_subject":"インパクター","subitem_subject_scheme":"Other"},{"subitem_subject":"クレーター形成","subitem_subject_scheme":"Other"},{"subitem_subject":"Moon","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"crustal dichotomy","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"rotational dynamics","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"moment of inertia","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"structural basin","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"lunar crustal thickness","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"impactor","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"cratering","subitem_subject_language":"en","subitem_subject_scheme":"Other"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"conference paper","resourceuri":"http://purl.org/coar/resource_type/c_5794"}]},"item_title":"Crustal dichotomy and reorientation of the Moon as a consequence of a leading-trailing asymmetry in the cratering rate","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Crustal dichotomy and reorientation of the Moon as a consequence of a leading-trailing asymmetry in the cratering rate","subitem_title_language":"en"}]},"item_type_id":"5","owner":"1","path":["1792","1891"],"pubdate":{"attribute_name":"公開日","attribute_value":"2015-03-26"},"publish_date":"2015-03-26","publish_status":"0","recid":"20579","relation_version_is_last":true,"title":["Crustal dichotomy and reorientation of the Moon as a consequence of a leading-trailing asymmetry in the cratering rate"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-06-21T03:48:17.006487+00:00"}