WEKO3
アイテム
{"_buckets": {"deposit": "ea3bfdc8-4e17-4a34-86f9-376219d468aa"}, "_deposit": {"id": "20464", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "20464"}, "status": "published"}, "_oai": {"id": "oai:soar-ir.repo.nii.ac.jp:00020464", "sets": ["1170"]}, "author_link": ["107420", "107421"], "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": "Response of slope-shelf-nearshore systems to relative sea-level changes in the Miocene Aoki and Ogawa formations, Northern Fossa Magna region, central Japan"}]}, "item_6_biblio_info_6": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1992-04-15", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "4", "bibliographicPageEnd": "354", "bibliographicPageStart": "337", "bibliographicVolumeNumber": "98", "bibliographic_titles": [{"bibliographic_title": "地質学雑誌"}]}]}, "item_6_description_20": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "The Northern Fossa Magna region is situated at the junction of the Northeast and Southwest Honshu arcs. The Middle to Late Miocene Aoki and Ogawa formations occur in the Komiji Syncline area in the southern part of the Northern Fossa Magna region. The Aoki and Ogawa formations in the study area are divided into thirteen sedimentary facies. On the basis of facies analysis, the upper part of the Aoki Formation was deposited at continental slope and outer shelf, while the Ogawa Formation was at inner shelf and various coastal environments. Within these formations there are conglomerate beds deposited on the transgressive surfaces.\u003cbr/\u003eThe assemblages of sedimentary facies are characterized either by coarsening-upward or fining-upward features. The coarsening-upward facies assemblage resulted from the regression in a coastal environment, whereas the fining-upward facies assemblage from the regression in a barrirer environment. The distribution and stacking pattern of these regressive facies successions reveal a progradational system of coastal and strand-plain environments, followed by an aggradational system of coastal and barrier island environments and then by a repeat of the progradation-aggradation cycle. The progradational system along the coast resulted from a decrease in accommodation, whereas the aggradational system along the coast depended on an increase in accommodation. Changes in accommodation are equivalent to relative sea-level changes. Therefore, the relative sea-level curve can be described from the changes of accommodation.\u003cbr/\u003eThe relative sea-level of this area changed in response to eustacy, estimated from the Haq curve. Therefore, the framework of sequence stratigraphy may be applicable to this and other basins of this active region. Two sequence boundaries can be identified in the study area. The lower sequence boundary is placed between the Aoki Formation and the Ogawa Formation, and the other can be identified in the middle part of the Ogawa Formation. These correspond to the 10.5Ma and 8.2Ma sequence boundaries of the eustacy curve, respectively.\u003cbr/\u003eAccommodation is a function of bouth eustacy and subsidence. The subsidence of the basin can be calculated from the accommodation and eustacy. This basin subsided during deposition of the Ogawa Formation (from 10Ma to 6Ma) at a rate of 60m per 1Ma Uncorrected for compaction.", "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": "地質学雑誌.98(4):337-354(1992)", "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, 康一", "subitem_link_url": "http://soar-rd.shinshu-u.ac.jp/profile/ja.jpDmOUkh.html"}]}, "item_6_publisher_4": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "日本地質学会"}]}, "item_6_relation_48": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_name": [{"subitem_relation_name_text": "10.5575/geosoc.98.337"}], "subitem_relation_type_id": {"subitem_relation_type_id_text": "https://doi.org/10.5575/geosoc.98.337", "subitem_relation_type_select": "DOI"}}]}, "item_6_rights_62": {"attribute_name": "権利", "attribute_value_mlt": [{"subitem_rights": "© 日本地質学会"}]}, "item_6_select_64": {"attribute_name": "著者版フラグ", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_6_source_id_35": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0016-7630", "subitem_source_identifier_type": "ISSN"}]}, "item_6_source_id_39": {"attribute_name": "NII ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0016-7630", "subitem_source_identifier_type": "ISSN"}]}, "item_6_source_id_40": {"attribute_name": "書誌レコードID", "attribute_value_mlt": [{"subitem_source_identifier": "AN00141768", "subitem_source_identifier_type": "NCID"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "西村, 瑞恵"}], "nameIdentifiers": [{"nameIdentifier": "107420", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "保柳, 康一"}], "nameIdentifiers": [{"nameIdentifier": "107421", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2019-02-22"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "26400486_x5.pdf", "filesize": [{"value": "4.5 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensefree": "© 日本地質学会", "licensetype": "license_note", "mimetype": "application/pdf", "size": 4500000.0, "url": {"label": "26400486_x5.pdf", "url": "https://soar-ir.repo.nii.ac.jp/record/20464/files/26400486_x5.pdf"}, "version_id": "7b4521bd-3ec7-4a54-8d8f-5930fd05b927"}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "sedimentary facies", "subitem_subject_scheme": "Other"}, {"subitem_subject": "sedimentary system", "subitem_subject_scheme": "Other"}, {"subitem_subject": "accommodation", "subitem_subject_scheme": "Other"}, {"subitem_subject": "sequence stratigraphy", "subitem_subject_scheme": "Other"}, {"subitem_subject": "transgressive surface", "subitem_subject_scheme": "Other"}, {"subitem_subject": "basin analysis", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Miocene", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Northern Fossa Magna", "subitem_subject_scheme": "Other"}]}, "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": "journal article", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "陸棚斜面-陸棚-沿岸の堆積システムの変遷と相対的海水準変動 : 北部フォッサマグナ地域中新統青木層・小川層のシークェンス層序学", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "陸棚斜面-陸棚-沿岸の堆積システムの変遷と相対的海水準変動 : 北部フォッサマグナ地域中新統青木層・小川層のシークェンス層序学", "subitem_title_language": "ja"}]}, "item_type_id": "6", "owner": "1", "path": ["1170"], "permalink_uri": "http://hdl.handle.net/10091/00021222", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2019-02-22"}, "publish_date": "2019-02-22", "publish_status": "0", "recid": "20464", "relation": {}, "relation_version_is_last": true, "title": ["陸棚斜面-陸棚-沿岸の堆積システムの変遷と相対的海水準変動 : 北部フォッサマグナ地域中新統青木層・小川層のシークェンス層序学"], "weko_shared_id": -1}
陸棚斜面-陸棚-沿岸の堆積システムの変遷と相対的海水準変動 : 北部フォッサマグナ地域中新統青木層・小川層のシークェンス層序学
http://hdl.handle.net/10091/00021222
http://hdl.handle.net/10091/00021222852237cc-4d18-4095-afeb-dd74b551a618
名前 / ファイル | ライセンス | アクション |
---|---|---|
26400486_x5.pdf (4.5 MB)
|
|
Item type | 学術雑誌論文 / Journal Article(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2019-02-22 | |||||
タイトル | ||||||
言語 | ja | |||||
タイトル | 陸棚斜面-陸棚-沿岸の堆積システムの変遷と相対的海水準変動 : 北部フォッサマグナ地域中新統青木層・小川層のシークェンス層序学 | |||||
言語 | ||||||
言語 | jpn | |||||
DOI | ||||||
識別子タイプ | DOI | |||||
関連識別子 | https://doi.org/10.5575/geosoc.98.337 | |||||
関連名称 | 10.5575/geosoc.98.337 | |||||
キーワード | ||||||
主題 | sedimentary facies, sedimentary system, accommodation, sequence stratigraphy, transgressive surface, basin analysis, Miocene, Northern Fossa Magna | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | journal article | |||||
その他(別言語等)のタイトル | ||||||
その他のタイトル | Response of slope-shelf-nearshore systems to relative sea-level changes in the Miocene Aoki and Ogawa formations, Northern Fossa Magna region, central Japan | |||||
著者 |
西村, 瑞恵
× 西村, 瑞恵× 保柳, 康一 |
|||||
信州大学研究者総覧へのリンク | ||||||
氏名 | 保柳, 康一 | |||||
URL | http://soar-rd.shinshu-u.ac.jp/profile/ja.jpDmOUkh.html | |||||
出版者 | ||||||
出版者 | 日本地質学会 | |||||
引用 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 地質学雑誌.98(4):337-354(1992) | |||||
書誌情報 |
地質学雑誌 巻 98, 号 4, p. 337-354, 発行日 1992-04-15 |
|||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The Northern Fossa Magna region is situated at the junction of the Northeast and Southwest Honshu arcs. The Middle to Late Miocene Aoki and Ogawa formations occur in the Komiji Syncline area in the southern part of the Northern Fossa Magna region. The Aoki and Ogawa formations in the study area are divided into thirteen sedimentary facies. On the basis of facies analysis, the upper part of the Aoki Formation was deposited at continental slope and outer shelf, while the Ogawa Formation was at inner shelf and various coastal environments. Within these formations there are conglomerate beds deposited on the transgressive surfaces.<br/>The assemblages of sedimentary facies are characterized either by coarsening-upward or fining-upward features. The coarsening-upward facies assemblage resulted from the regression in a coastal environment, whereas the fining-upward facies assemblage from the regression in a barrirer environment. The distribution and stacking pattern of these regressive facies successions reveal a progradational system of coastal and strand-plain environments, followed by an aggradational system of coastal and barrier island environments and then by a repeat of the progradation-aggradation cycle. The progradational system along the coast resulted from a decrease in accommodation, whereas the aggradational system along the coast depended on an increase in accommodation. Changes in accommodation are equivalent to relative sea-level changes. Therefore, the relative sea-level curve can be described from the changes of accommodation.<br/>The relative sea-level of this area changed in response to eustacy, estimated from the Haq curve. Therefore, the framework of sequence stratigraphy may be applicable to this and other basins of this active region. Two sequence boundaries can be identified in the study area. The lower sequence boundary is placed between the Aoki Formation and the Ogawa Formation, and the other can be identified in the middle part of the Ogawa Formation. These correspond to the 10.5Ma and 8.2Ma sequence boundaries of the eustacy curve, respectively.<br/>Accommodation is a function of bouth eustacy and subsidence. The subsidence of the basin can be calculated from the accommodation and eustacy. This basin subsided during deposition of the Ogawa Formation (from 10Ma to 6Ma) at a rate of 60m per 1Ma Uncorrected for compaction. | |||||
資源タイプ(コンテンツの種類) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Article | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0016-7630 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00141768 | |||||
権利 | ||||||
権利情報 | © 日本地質学会 | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |