{"created":"2021-03-01T06:20:17.454252+00:00","id":17248,"links":{},"metadata":{"_buckets":{"deposit":"53081da5-a4b5-4643-bcc0-1ecb49787b1e"},"_deposit":{"id":"17248","owners":[],"pid":{"revision_id":0,"type":"depid","value":"17248"},"status":"published"},"_oai":{"id":"oai:soar-ir.repo.nii.ac.jp:00017248","sets":["1628:1674:1678"]},"author_link":["49096"],"item_10_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1951-07","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"1","bibliographicPageEnd":"25","bibliographicPageStart":"9","bibliographicVolumeNumber":"1","bibliographic_titles":[{"bibliographic_title":"信州大學紀要"}]}]},"item_10_description_20":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"1) フォッサ・マグナ西部における内陸性堆積物,地殻運動,火山活動,地形発達史等を比較することにより,第四紀地殻運動により時代的区分を試み,かかる運動の特性により,表現される現象に注目し,侵蝕区時代,地塊化時代,現河川による礫層形成時代とした。2) フォッサ・マグナ内部における対比基準として第6表の如きタイプを定めた。比較されている地質年代は暫定であり,その細分は本邦標準小区分のa,b等とは異るもので単に同時性を示す程度のものであるから(a),(b) とした。3) 地塊運動期として次の4回が顕著に認められる。F1先塩川層群変動(dl II前期)F2後塩川層群変動(dl II後期)F3先旧河床礫変動(du I)F4後旧河床礫変動(du I)4) 気候史に就いてはdu II (c)~(a₁)の唐花見泥炭層より, du I後期の古溜泥炭層の間が寒く,塩川バイオータも寒い様であるが,それ以外に気候資料はない,氷期はdu IのMenyanthes層準に成るらしいととは他の機会に説明し度い。","subitem_description_type":"Abstract"},{"subitem_description":"In this paper on the geologic and physiographic developments of thewestern parts of the Fossa Magna, the crustal movements were taken as a chronological standards. It is very difficult to correlate the geological events in this district with the chronological standard of Japan, because of the remoteness from the marine deposits. Therefore the local chronological standard shoud be established, for the FossaMagna. The Quarternary Era was divided into 3 epochs of the crustal movements,as follows;
as follows;ⅠEpoch of Denudation ⅡEpoch of Block Movement ⅢEpoch of Deposition of Fanglomerates As the products of the first block movement the epoch, the land was raised, the thick deposits of gravel formed large scaled fan outside the mountains. A lower part of the gravel was raised by the last faulting(f4), and was called \"Older Gravels\". The sandards of crrelation in the Fossa Magna were enumerated in Table 8, and the increase and the decrease of the relief of the land is also schematized in it.","subitem_description_type":"Abstract"}]},"item_10_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_10_description_5":{"attribute_name":"引用","attribute_value_mlt":[{"subitem_description":"信州大學紀要 1(1): 9-25(1951)","subitem_description_type":"Other"}]},"item_10_publisher_4":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"信州大学"}]},"item_10_source_id_40":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00219843","subitem_source_identifier_type":"NCID"}]},"item_1627890569677":{"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_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"小林, 國夫"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2015-09-28"}],"displaytype":"detail","filename":"Shinshu_Bulletin01-02.pdf","filesize":[{"value":"1.4 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"Shinshu_Bulletin01-02.pdf","url":"https://soar-ir.repo.nii.ac.jp/record/17248/files/Shinshu_Bulletin01-02.pdf"},"version_id":"193e106d-3079-4b98-8ada-91ab5c018762"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"フォッサ・マグナ西部附近における第四紀編年","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"フォッサ・マグナ西部附近における第四紀編年","subitem_title_language":"ja"},{"subitem_title":"Quaternary Chronology of the Western Parts of the Fossa Magna","subitem_title_language":"en"}]},"item_type_id":"10","owner":"1","path":["1678"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2010-02-12"},"publish_date":"2010-02-12","publish_status":"0","recid":"17248","relation_version_is_last":true,"title":["フォッサ・マグナ西部附近における第四紀編年"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-01-18T01:35:08.924208+00:00"}