WEKO3
インデックスリンク
アイテム
{"_buckets": {"deposit": "34b582f1-7f31-4df0-8b13-08e23f1769a8"}, "_deposit": {"created_by": 3, "id": "29305", "owners": [3], "pid": {"revision_id": 0, "type": "depid", "value": "29305"}, "status": "published"}, "_oai": {"id": "oai:kanazawa-u.repo.nii.ac.jp:00029305", "sets": ["1981"]}, "author_link": ["50306", "50305", "50304", "50303", "50307", "50302", "2915", "15862"], "item_4_biblio_info_8": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2007-03-01", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "5-6", "bibliographicPageEnd": "592", "bibliographicPageStart": "585", "bibliographicVolumeNumber": "29", "bibliographic_titles": [{"bibliographic_title": "Journal of Asian Earth Sciences"}]}]}, "item_4_creator_33": {"attribute_name": "著者別表示", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "塚脇, 真二"}], "nameIdentifiers": [{"nameIdentifier": "2915", "nameIdentifierScheme": "WEKO"}, {"nameIdentifier": "00222133", "nameIdentifierScheme": "e-Rad", "nameIdentifierURI": "https://kaken.nii.ac.jp/ja/search/?qm=00222133"}]}]}, "item_4_description_21": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "The depositional facies and radiocarbon ages of a long Holocene sediment core (KS) from Cambodia are reported here to clarify the sedimentary environments of the Mekong River delta system at the time of Holocene maximum flooding by the sea. The 30.7-m-long KS core, from the upper Mekong River lowland about 20 km southeast of Phnom Penh, penetrated five depositional facies, A to E in ascending order. Facies A is cross-laminated fluvial sand. Facies B is laminated, very fine sand with mud drapes.Facies C to E are salt marsh, flood-plain and natural-levee deposits, characterized by a succession of peat, organic clay, and reddish brown silt. Facies B dates to 9.0 to 7.5 ka and is interpreted as aggradational tidal deposits, 16.5 m thick, deposited during a rapid rise of sea level; these deposits became overlain by an accumulation of salt marsh and flood-plain deposits during the subsequent period of slowly rising and then falling sea level. The maximum flooding surface lies in the Facies B interval. The presence of tidal deposits implies that the core site, about 230 km inland from the present river mouth, was near the shoreline and experienced strong tidal influences during the early Holocene.© 2006 Elsevier Ltd. All rights reserved.", "subitem_description_type": "Abstract"}]}, "item_4_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.24517/00029292", "subitem_identifier_reg_type": "JaLC"}]}, "item_4_publisher_17": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "Elsevier"}]}, "item_4_relation_12": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "https://doi.org/10.1016/j.jseaes.2006.03.009", "subitem_relation_type_select": "DOI"}}]}, "item_4_relation_28": {"attribute_name": "関連URI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "http://www.elsevier.com/locate/issn/13679120", "subitem_relation_type_select": "URI"}}]}, "item_4_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "1367-9120", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Tamura, Toru"}], "nameIdentifiers": [{"nameIdentifier": "50302", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Saito, Yoshiki"}], "nameIdentifiers": [{"nameIdentifier": "50303", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Sieng, Sotham"}], "nameIdentifiers": [{"nameIdentifier": "50304", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Ben, Bunnarin"}], "nameIdentifiers": [{"nameIdentifier": "50305", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Kong, Meng"}], "nameIdentifiers": [{"nameIdentifier": "50306", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Choup, Sokuntheara"}], "nameIdentifiers": [{"nameIdentifier": "50307", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Tsukawaki, Shinji"}], "nameIdentifiers": [{"nameIdentifier": "15862", "nameIdentifierScheme": "WEKO"}, {"nameIdentifier": "00222133", "nameIdentifierScheme": "e-Rad", "nameIdentifierURI": "https://kaken.nii.ac.jp/ja/search/?qm=00222133"}, {"nameIdentifier": "00222133", "nameIdentifierScheme": "金沢大学研究者情報", "nameIdentifierURI": "http://ridb.kanazawa-u.ac.jp/public/detail.php?kaken=00222133"}, {"nameIdentifier": "00222133", "nameIdentifierScheme": "研究者番号", "nameIdentifierURI": "https://nrid.nii.ac.jp/nrid/1000000222133"}]}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2017-10-05"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "CambodiaKScore.pdf", "filesize": [{"value": "1.0 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_11", "mimetype": "application/pdf", "size": 1000000.0, "url": {"label": "CambodiaKScore.pdf", "url": "https://kanazawa-u.repo.nii.ac.jp/record/29305/files/CambodiaKScore.pdf"}, "version_id": "5ed1046c-0331-4de4-bcf8-32141b31be86"}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "Aggradation", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Delta", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Highstand Mud drapes", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Peat", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Regression", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Sea-level rise", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Transgression", "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": "journal article", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "Depositional facies and radiocarbon ages of a drill core from the Mekong River lowland near Phnom Penh, Cambodia: evidence for tidal sedimentation at the time of Holocene maximum flooding", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Depositional facies and radiocarbon ages of a drill core from the Mekong River lowland near Phnom Penh, Cambodia: evidence for tidal sedimentation at the time of Holocene maximum flooding"}]}, "item_type_id": "4", "owner": "3", "path": ["1981"], "permalink_uri": "https://doi.org/10.24517/00029292", "pubdate": {"attribute_name": "公開日", "attribute_value": "2017-10-05"}, "publish_date": "2017-10-05", "publish_status": "0", "recid": "29305", "relation": {}, "relation_version_is_last": true, "title": ["Depositional facies and radiocarbon ages of a drill core from the Mekong River lowland near Phnom Penh, Cambodia: evidence for tidal sedimentation at the time of Holocene maximum flooding"], "weko_shared_id": 3}
Depositional facies and radiocarbon ages of a drill core from the Mekong River lowland near Phnom Penh, Cambodia: evidence for tidal sedimentation at the time of Holocene maximum flooding
https://doi.org/10.24517/00029292
https://doi.org/10.24517/00029292749f3458-8e53-442e-9a86-b4c07a8564c3
名前 / ファイル | ライセンス | アクション |
---|---|---|
CambodiaKScore.pdf (1.0 MB)
|
Item type | 学術雑誌論文 / Journal Article(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2017-10-05 | |||||
タイトル | ||||||
タイトル | Depositional facies and radiocarbon ages of a drill core from the Mekong River lowland near Phnom Penh, Cambodia: evidence for tidal sedimentation at the time of Holocene maximum flooding | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | journal article | |||||
ID登録 | ||||||
ID登録 | 10.24517/00029292 | |||||
ID登録タイプ | JaLC | |||||
著者 |
Tamura, Toru
× Tamura, Toru× Saito, Yoshiki× Sieng, Sotham× Ben, Bunnarin× Kong, Meng× Choup, Sokuntheara× Tsukawaki, Shinji |
|||||
著者別表示 |
塚脇, 真二
× 塚脇, 真二 |
|||||
書誌情報 |
Journal of Asian Earth Sciences 巻 29, 号 5-6, p. 585-592, 発行日 2007-03-01 |
|||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 1367-9120 | |||||
DOI | ||||||
識別子タイプ | DOI | |||||
関連識別子 | https://doi.org/10.1016/j.jseaes.2006.03.009 | |||||
出版者 | ||||||
出版者 | Elsevier | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The depositional facies and radiocarbon ages of a long Holocene sediment core (KS) from Cambodia are reported here to clarify the sedimentary environments of the Mekong River delta system at the time of Holocene maximum flooding by the sea. The 30.7-m-long KS core, from the upper Mekong River lowland about 20 km southeast of Phnom Penh, penetrated five depositional facies, A to E in ascending order. Facies A is cross-laminated fluvial sand. Facies B is laminated, very fine sand with mud drapes.Facies C to E are salt marsh, flood-plain and natural-levee deposits, characterized by a succession of peat, organic clay, and reddish brown silt. Facies B dates to 9.0 to 7.5 ka and is interpreted as aggradational tidal deposits, 16.5 m thick, deposited during a rapid rise of sea level; these deposits became overlain by an accumulation of salt marsh and flood-plain deposits during the subsequent period of slowly rising and then falling sea level. The maximum flooding surface lies in the Facies B interval. The presence of tidal deposits implies that the core site, about 230 km inland from the present river mouth, was near the shoreline and experienced strong tidal influences during the early Holocene.© 2006 Elsevier Ltd. All rights reserved. | |||||
関連URI | ||||||
識別子タイプ | URI | |||||
関連識別子 | http://www.elsevier.com/locate/issn/13679120 |