{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1361699995564659200.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/s0025-3227(01)00165-7"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0025322701001657?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0025322701001657?httpAccept=text/plain"}}],"dc:title":[{"@value":"Sedimentary facies of the tide-dominated paleo-Changjiang (Yangtze) estuary during the last transgression"}],"description":[{"notation":[{"@value":"Abstract   A large estuary was formed by marine inundation of the paleo-Changjiang (Yangtze) incised valley during the transgression after the Last Glacial Maximum. This paper presents the sedimentary facies and architecture of the estuary fill, based on the analysis of three sediment cores (CM97, JS98, and HQ98) obtained from the present Changjiang delta plain.  Estuary fill deposits showing an upward-fining succession were grouped into five depositional facies: tidal river, distributary channel, muddy intertidal to subtidal flats, transgressive lag, and estuary front, based on sedimentary textures, lithology, and physical sedimentary structures. Sand–mud couplets are common in these deposits, indicating that tides played a significant role in producing these sedimentary structures and that the estuary type was tide-dominated. Some of the successive sand–mud couplets probably recorded neap-spring cycles as well as semidiurnal tidal cycles.  The nature of the estuary was very different from other representative tide-dominated estuaries in sediment facies, its distribution, and sediment source for estuarine fill. Unlike the other estuaries that receive sediments mainly from the sea, the paleo-Changjiang estuarine fill deposits were supplied largely from the river. This difference would also have a great influence on the sedimentological and morphological component in the estuary. The sediment distribution of the estuary showed fining-seaward and estuary-mouth sand bodies fed by marine-source sand were absent. The architecture model of tide-dominated estuaries should be divided into two types by the degree of fluvial sediment supply. The paleo-Changjiang estuary shows a good example for an estuary of large rivers."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699995564659206","@type":"Researcher","foaf:name":[{"@value":"Kazuaki Hori"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995564659200","@type":"Researcher","foaf:name":[{"@value":"Yoshiki Saito"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995564659204","@type":"Researcher","foaf:name":[{"@value":"Quanhong Zhao"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995564659203","@type":"Researcher","foaf:name":[{"@value":"Xinrong Cheng"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995564659201","@type":"Researcher","foaf:name":[{"@value":"Pinxian Wang"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995564659205","@type":"Researcher","foaf:name":[{"@value":"Yoshio Sato"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995564659202","@type":"Researcher","foaf:name":[{"@value":"Congxian Li"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00253227"}],"prism:publicationName":[{"@value":"Marine Geology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2001-07","prism:volume":"177","prism:number":"3-4","prism:startingPage":"331","prism:endingPage":"351"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0025322701001657?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0025322701001657?httpAccept=text/plain"}],"createdAt":"2002-07-25","modifiedAt":"2025-09-20","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050013397240385536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Upper and lower plane bed definitions revised"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232469002624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Differences in radiocarbon ages among molluscan shells, plant materials, and total organic carbon: An example from the paleo-Changjiang incised-valley fill, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233286387840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Variations of East Asian summer monsoon since the last deglaciation based on Mg/Ca and oxygen isotope of planktic foraminifera in the northern East China Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005517247316864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Early to middle Holocene development of the Tsushima Warm Current based on benthic and planktonic foraminifera in the Nakdong River delta (southeast Korea)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168737465344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Organic geochemical evidence of past changes in hydro- and sediment-dynamic processes at river mouths: A case study of Holocene sedimentary records in the Changjiang River delta, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707396573568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Initiation of the Changjiang (Yangtze) delta and its response to the mid-Holocene sea level change"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707445047552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The sedimentary evolution of Yangtze River delta since MIS3: A new chronology evidence revealed by OSL dating"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285713317807360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tide- and River-Generated Mud Pebbles from the Fluvial To Marine Transition Zone of the Mekong River Delta, Vietnam"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643738187776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coastal development in southwestern Bangladesh: understanding the interplay between storms and sea level rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182056140800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional evolution of the Yangtze River mouth, China during the Holocene: impacts of sea level, climate and human activity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118691115392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Latest Pleistocene to Holocene stratigraphic record and evolution of the Paleo-Mekong incised valley, Vietnam"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640994116480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Application of MASW technology to identification of tidal flat stratigraphy and its geoenvironmental interpretation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657419375360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sedimentary stratigraphy of natural intertidal flats with various characteristics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848663272628736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sedimentation History of Sandbars in Flood-Tidal Delta Evaluated by Seismic Method in Lake Tofutsu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238323968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Uplift of the Himalayas and Tibetan Plateau and large river deltas in Asia: their characteristics and Holocene evolution"},{"@language":"ja","@value":"ヒマラヤーチベットの隆起とアジアの大規模デルタ：デルタの特徴と完新世における進展"},{"@language":"ja-Kana","@value":"ヒマラヤ チベット ノ リュウキ ト アジア ノ ダイキボ デルタ デルタ ノ トクチョウ ト カンシン セイ ニ オケル シンテン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206497039360","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Coastal depositional systems and sea-level change"},{"@language":"ja","@value":"沿岸域の堆積システムと海水準変動"},{"@value":"2009年度日本第四紀学会学術賞受賞記念論文 沿岸域の堆積システムと海水準変動"},{"@language":"ja-Kana","@value":"2009ネンド ニホン ダイ4キ ガッカイ ガクジュツショウ ジュショウ キネン ロンブン エンガンイキ ノ タイセキ システム ト ウミ スイジュン ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681473547648","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Holocene evolution of the Kumozu River delta, Mie Prefecture, central Japan"},{"@language":"ja","@value":"完新世における三重県，雲出川デルタの発達過程"},{"@value":"Holocene evolution of the Kumozu delta, Mie Prefecture, Central Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/s0025-3227(01)00165-7"},{"@type":"OPENAIRE","@value":"doi_dedup___::d2b28b54bd60b257ab0c04da3d18a189"},{"@type":"CROSSREF","@value":"10.1029/2009pa001891_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.1016/j.sandf.2012.05.003_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.1016/j.csr.2020.104189_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00481-8_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.2112/jcoastres-d-15-00113.1_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.1177/03091333211046189_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.5575/geosoc.111.717_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.4116/jaqua.50.95_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.1016/j.margeo.2008.03.007_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.1016/j.quaint.2017.07.037_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.1016/j.margeo.2020.106406_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.4116/jaqua.49.201_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.1016/j.palaeo.2013.07.026_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.1016/j.quaint.2018.11.040_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.2110/jsr.2018.54_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.1016/j.quageo.2018.03.010_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"},{"@type":"CROSSREF","@value":"10.1016/j.earscirev.2018.08.012_references_DOI_DjKLCcesrHXI3P1pKJozMLbu77Z"}]}