Matches in SemOpenAlex for { <https://semopenalex.org/work/W2044331508> ?p ?o ?g. }
Showing items 1 to 63 of
63
with 100 items per page.
- W2044331508 endingPage "156" @default.
- W2044331508 startingPage "139" @default.
- W2044331508 abstract "Abstract Tidal inlet sediments make up a significant portion of most barrier island complexes. Inlet-affiliated sedimentary units usually include an ebb-tidal delta (seaward shoal), a flood-tidal delta (landward shoal) and inlet-fill sequences created by inlet migration and recurved spit growth. The morphological components of ebb-tidal deltas include a main ebb channel flanked by linear bars on either side and a terminal sand lobe at the seaward end. This channel is bordered by a platform of sand dominated by swash bars which is separated from adjacent barrier beaches by marginal flood channels. The ebb-delta sand body is coarser-grained than other sedimentary units of the inlet and contains polymodal cross-bedding with a slight ebb dominance. Flood-tidal deltas consist of a flood ramp and bifurcating flood channels o the seaward side, which are dominated by flood currents and flood-oriented sand waves, and ebb shields, ebb spits and spillover lobes on the landward side, which contain an abundance of ebb-oriented bedforms. A proposed stratigraphic sequence for a typical flood-tidal delta contains bidirectional, large-scale crossbedded sand at the base, predominantly large-scale (flood-oriented) crossbedded sand in the middle, and finer-grained tidal flat and marsh sediment at the top. Inlets migrate at rates that vary from a few to several tens of meters per year, depending upon such variables as rate of longshore sediment transport and depth of the inlet. Inlet-fill sequences, which fine upward, contain coarse, bidirectional crossbedded sediments at the base, polydirectional crossbedded sands in the middle, and finer-grained aeolian sand at the top. Both tidal-delta morphology and relative size and abundance of ebb- and flood-tidal deltas are considerably different in different oceanographic settings. Microtidal (tidal range T.R. = 0–2 m) areas tend to have smaller ebb-tidal deltas and larger flood-tidal deltas; whereas, mesotidal (T.R. = 2–4 m) areas show just the opposite trend. Large waves tend to inhibit the development of ebb-tidal deltas and accentuate the growth of flood-tidal deltas." @default.
- W2044331508 created "2016-06-24" @default.
- W2044331508 creator A5008457309 @default.
- W2044331508 date "1980-04-01" @default.
- W2044331508 modified "2023-10-04" @default.
- W2044331508 title "General morphology and sediment patterns in tidal inlets" @default.
- W2044331508 cites W1999340939 @default.
- W2044331508 doi "https://doi.org/10.1016/0037-0738(80)90009-3" @default.
- W2044331508 hasPublicationYear "1980" @default.
- W2044331508 type Work @default.
- W2044331508 sameAs 2044331508 @default.
- W2044331508 citedByCount "253" @default.
- W2044331508 countsByYear W20443315082012 @default.
- W2044331508 countsByYear W20443315082013 @default.
- W2044331508 countsByYear W20443315082014 @default.
- W2044331508 countsByYear W20443315082015 @default.
- W2044331508 countsByYear W20443315082016 @default.
- W2044331508 countsByYear W20443315082017 @default.
- W2044331508 countsByYear W20443315082018 @default.
- W2044331508 countsByYear W20443315082019 @default.
- W2044331508 countsByYear W20443315082020 @default.
- W2044331508 countsByYear W20443315082021 @default.
- W2044331508 countsByYear W20443315082022 @default.
- W2044331508 countsByYear W20443315082023 @default.
- W2044331508 crossrefType "journal-article" @default.
- W2044331508 hasAuthorship W2044331508A5008457309 @default.
- W2044331508 hasConcept C111368507 @default.
- W2044331508 hasConcept C114793014 @default.
- W2044331508 hasConcept C127313418 @default.
- W2044331508 hasConcept C151730666 @default.
- W2044331508 hasConcept C201289731 @default.
- W2044331508 hasConcept C2816523 @default.
- W2044331508 hasConcept C2992357698 @default.
- W2044331508 hasConcept C499950583 @default.
- W2044331508 hasConceptScore W2044331508C111368507 @default.
- W2044331508 hasConceptScore W2044331508C114793014 @default.
- W2044331508 hasConceptScore W2044331508C127313418 @default.
- W2044331508 hasConceptScore W2044331508C151730666 @default.
- W2044331508 hasConceptScore W2044331508C201289731 @default.
- W2044331508 hasConceptScore W2044331508C2816523 @default.
- W2044331508 hasConceptScore W2044331508C2992357698 @default.
- W2044331508 hasConceptScore W2044331508C499950583 @default.
- W2044331508 hasIssue "1-3" @default.
- W2044331508 hasLocation W20443315081 @default.
- W2044331508 hasOpenAccess W2044331508 @default.
- W2044331508 hasPrimaryLocation W20443315081 @default.
- W2044331508 hasRelatedWork W1525181149 @default.
- W2044331508 hasRelatedWork W2013600999 @default.
- W2044331508 hasRelatedWork W2026415010 @default.
- W2044331508 hasRelatedWork W2040450918 @default.
- W2044331508 hasRelatedWork W2110311992 @default.
- W2044331508 hasRelatedWork W2147275033 @default.
- W2044331508 hasRelatedWork W2165791835 @default.
- W2044331508 hasRelatedWork W2782700902 @default.
- W2044331508 hasRelatedWork W3138855034 @default.
- W2044331508 hasRelatedWork W70942039 @default.
- W2044331508 hasVolume "26" @default.
- W2044331508 isParatext "false" @default.
- W2044331508 isRetracted "false" @default.
- W2044331508 magId "2044331508" @default.
- W2044331508 workType "article" @default.