{"refrec":{"BRefID":246360,"RR":"Dalrymple, R.W.; Mackay, D.A.; Ichaso, A.A.; Choi, K.S. (2012). Processes, morphodynamics, and facies of tide-dominated estuaries, in: Davis Jr., R.A. et al.Principles of tidal sedimentology. pp. 79-107. http://dx.doi.org/10.1007/978-94-007-0123-6_5","BEntID":238057,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":", in: Davis Jr., R.A. et al.Principles of tidal sedimentology. pp. 79-107. http://dx.doi.org/10.1007/978-94-007-0123-6_5","DocTypID":17,"DocType":"Book chapters","MarineFlag":0,"FreshFlag":1,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Dalrymple, R.W.; Mackay, D.A.; Ichaso, A.A.; Choi, K.S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Dalrymple, R.W. et al.","Englishabstract":"As defined in this chapter, an estuary forms during a shoreline transgression and then fills during a progradational phase that is transitional to a delta. The spatial distribution of processes, grain sizes and facies within tide-dominated estuaries is predictable in general terms. Tidal currents dominate sedimentation along the axis, with wave-dominated sedimentation occurring along the flanks of the estuary in its outer part. Tidal energy increases into the estuary but then decreases toward the tidal limit, with a gradual transition to river-dominated sedimentation at its head. The interaction of the tidal wave with the morphology of the estuary, and with river currents, causes the outer estuary to be flood-dominant, with a net landward movement of sand. By contrast, the inner estuary is ebb-dominant, creating a bedload convergence within the estuary. The axial sandy deposits are typically finest at this location. In transgressive-phase estuaries, the main channel shows a low—high—low pattern of sinuosity, with the tightest bends (sinuosity = 2.5) occurring at the bedload convergence. These bends experience neck cutoff in the transition to the progradational phase of estuary filling. The estuary-mouth region is characterized by cross-bedded sands deposited on elongate sand bars, although wave-generated structures can be important in some cases. Estuaries that are down-drift of major rivers have anomalously muddy outer estuarine deposits. Further landward, upper-flow-regime parallel lamination can be widespread. The margins of the inner estuary are flanked by muddy salt-marsh and tidal-flat deposits that can contain well-developed tidal rhythmites and evidence of seasonal variations in river discharge.","AbstractOtherLang":null,"BibLvlCode":"AM","StandardTitle":"Processes, morphodynamics, and facies of tide-dominated estuaries","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2012,"MonPub":null,"DateUpdate":"2015-05-29","DateCreate":"2015-05-04","SecASFANote":null,"ConfID":null,"PeerRev":0,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":0,"DOI":"10.1007/978-94-007-0123-6_5"},"refs":null,"anarec":{"AnaID":246360,"PubliDate":2012,"Pagination":"79-107","XtraPublOfAnaID":null,"ISBN":"978-94-007-0122-9","Volume":null,"Issue":null,"BRefMon":246359,"BRefMonRR":"Davis Jr., R.A.; Dalrymple, R.W. (Ed.) (2012). Principles of tidal sedimentology. Springer: New York, Heidelberg. ISBN 978-94-007-0122-9. 621 pp. http://dx.doi.org/10.1007/978-94-007-0123-6","BRefXtra":null,"BRefXtraRR":null,"SerBRefID":null,"SerRR":null,"StandardTitleSer":null,"ISSN":null,"AbbrevSer":null,"StandardTitleMon":"Principles of tidal sedimentology","StartPage":79,"Pages":29,"ToPubliDate":null,"BRefBibLvlCode":"M","SerNotes":null,"AutString":"Davis Jr., R.A.; Dalrymple, R.W. (Ed.)"},"monrec":null,"serrec":null,"relations":null,"relationsRev":null,"addrec":null,"othpubs":null,"ownerships":null,"authors":[{"AutName":"Dalrymple","Firstname":"Robert","Initials":"R.W.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":238057,"AutID":83450,"OrderNr":1,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null},{"AutName":"Mackay","Firstname":"Duncan","Initials":"D.A.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":238057,"AutID":193652,"OrderNr":2,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null},{"AutName":"Ichaso","Firstname":"Aitor","Initials":"A.A.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":238057,"AutID":193653,"OrderNr":3,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null},{"AutName":"Choi","Firstname":"Kyungsik","Initials":"K.S.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":238057,"AutID":193654,"OrderNr":4,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null}],"mapdetails":null,"datasets":null,"monographs":null,"monparts":null,"serparts":null,"BEntOpen":null,"BEntPrivate":null,"availability":[{"BInstID":271003,"LibID":36,"BRefID":246360,"EmbargoDate":null,"FullEmbargoDate":null,"PhysMedID":16,"hasOCRd":1,"ShelfLocCode":"271003","RFID":null,"PaidValue":null,"Medium":"Server","Description":"Interne VLIZ documenten","Acronym":"VLIZ","Library":"Vlaams Instituut voor de Zee","DutchTerm":"Non-open access","URL":null,"ClassifID":228,"Classification":"Non-open access","ReqLink":1,"ClassifTypID":3,"URLLocation":"https://www.vliz.be/imisdocs/publications/","SubDir":1,"InternalReq":1,"LoggedInReq":1,"Disclaimer":"Disclaimer_VLIZ_Intern","DutchDisclaimer":"
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