FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2034705058> ?p ?o ?g. }

• W2034705058 endingPage "24157" @default.
• W2034705058 startingPage "24141" @default.
• W2034705058 abstract "Clinoforms are the building blocks of prograding stratigraphic sequences. These sigmoid-shaped surfaces can be found forming today on modern deltas. Sedimentation rate profiles over the clinoform surface of these deltas show low rates of sediment accumulation on both topset and bottomset regions, with a maximum accumulation rate on the upper foreset region. We present a model for the formation of clinoforms that relies on the interpretation of modern clinoform sedimentation as a result of the distribution of shear stresses at the mouth of a river. Model clinoform surfaces are generated using an equation for the conservation of suspended sediment concentration, together with a conservation of fluid equation for simple time-averaged flow velocity fields. In the model, suspended sediment is adverted horizontally into a basin, and gravitational settling of sediment particles is counteracted by vertical turbulent diffusion. In shallow water, shear stresses are too large to allow deposition, and sediment bypasses the topset region. With increasing water depth, near-bed shear stresses decrease, and sediment is allowed to deposit at the foreset region, with gradually decreasing rates toward deeper water. This sedimentation pattern leads to progradation of the clinoform surfaces through time. The clinoform surfaces produced by the model capture the fundamental morphological characteristics of natural clinoforms. These include the gradual slope rollover at the topset and bottomset, steeper foreset slopes with increased grain size, and an increase in foreset slope through time as clinoforms prograde into deeper water. Because the parameters controlling the model clinoforms have a direct relation to physical quantities that can be measured in natural systems, the model is an important step toward unraveling the physical processes associated with these deposits." @default.
• W2034705058 created "2016-06-24" @default.
• W2034705058 creator A5012022118 @default.
• W2034705058 creator A5043382953 @default.
• W2034705058 creator A5043878489 @default.
• W2034705058 date "1998-10-10" @default.
• W2034705058 modified "2023-10-16" @default.
• W2034705058 title "Clinoform development by advection-diffusion of suspended sediment: Modeling and comparison to natural systems" @default.
• W2034705058 cites W1523973939 @default.
• W2034705058 cites W1530068409 @default.
• W2034705058 cites W1533766981 @default.
• W2034705058 cites W1909319766 @default.
• W2034705058 cites W192070839 @default.
• W2034705058 cites W1937848784 @default.
• W2034705058 cites W1964455165 @default.
• W2034705058 cites W1973935658 @default.
• W2034705058 cites W2000556437 @default.
• W2034705058 cites W2011183076 @default.
• W2034705058 cites W2014124878 @default.
• W2034705058 cites W2015525297 @default.
• W2034705058 cites W2025618090 @default.
• W2034705058 cites W2027182567 @default.
• W2034705058 cites W2029540335 @default.
• W2034705058 cites W2029629044 @default.
• W2034705058 cites W2032806381 @default.
• W2034705058 cites W2045606460 @default.
• W2034705058 cites W2047281401 @default.
• W2034705058 cites W2049757027 @default.
• W2034705058 cites W2053404357 @default.
• W2034705058 cites W2054443626 @default.
• W2034705058 cites W2055731461 @default.
• W2034705058 cites W2057365907 @default.
• W2034705058 cites W2058087073 @default.
• W2034705058 cites W2059472735 @default.
• W2034705058 cites W2063914863 @default.
• W2034705058 cites W2067319201 @default.
• W2034705058 cites W2085447624 @default.
• W2034705058 cites W2086046118 @default.
• W2034705058 cites W2086528171 @default.
• W2034705058 cites W2089762062 @default.
• W2034705058 cites W2102264361 @default.
• W2034705058 cites W2134806591 @default.
• W2034705058 cites W2142956098 @default.
• W2034705058 cites W2143212628 @default.
• W2034705058 cites W2149765269 @default.
• W2034705058 cites W2149966643 @default.
• W2034705058 cites W2153222505 @default.
• W2034705058 cites W2197113573 @default.
• W2034705058 cites W2246495653 @default.
• W2034705058 cites W2276415307 @default.
• W2034705058 cites W4206584024 @default.
• W2034705058 cites W4243487949 @default.
• W2034705058 cites W657231869 @default.
• W2034705058 doi "https://doi.org/10.1029/98jb01516" @default.
• W2034705058 hasPublicationYear "1998" @default.
• W2034705058 type Work @default.
• W2034705058 sameAs 2034705058 @default.
• W2034705058 citedByCount "175" @default.
• W2034705058 countsByYear W20347050582012 @default.
• W2034705058 countsByYear W20347050582013 @default.
• W2034705058 countsByYear W20347050582014 @default.
• W2034705058 countsByYear W20347050582015 @default.
• W2034705058 countsByYear W20347050582016 @default.
• W2034705058 countsByYear W20347050582017 @default.
• W2034705058 countsByYear W20347050582018 @default.
• W2034705058 countsByYear W20347050582019 @default.
• W2034705058 countsByYear W20347050582020 @default.
• W2034705058 countsByYear W20347050582021 @default.
• W2034705058 countsByYear W20347050582022 @default.
• W2034705058 countsByYear W20347050582023 @default.
• W2034705058 crossrefType "journal-article" @default.
• W2034705058 hasAuthorship W2034705058A5012022118 @default.
• W2034705058 hasAuthorship W2034705058A5043382953 @default.
• W2034705058 hasAuthorship W2034705058A5043878489 @default.
• W2034705058 hasBestOaLocation W20347050581 @default.
• W2034705058 hasConcept C109007969 @default.
• W2034705058 hasConcept C114793014 @default.
• W2034705058 hasConcept C126753816 @default.
• W2034705058 hasConcept C127313418 @default.
• W2034705058 hasConcept C16565575 @default.
• W2034705058 hasConcept C173209714 @default.
• W2034705058 hasConcept C2816523 @default.
• W2034705058 hasConcept C29941650 @default.
• W2034705058 hasConcept C39432304 @default.
• W2034705058 hasConcept C65589250 @default.
• W2034705058 hasConcept C87717796 @default.
• W2034705058 hasConceptScore W2034705058C109007969 @default.
• W2034705058 hasConceptScore W2034705058C114793014 @default.
• W2034705058 hasConceptScore W2034705058C126753816 @default.
• W2034705058 hasConceptScore W2034705058C127313418 @default.
• W2034705058 hasConceptScore W2034705058C16565575 @default.
• W2034705058 hasConceptScore W2034705058C173209714 @default.
• W2034705058 hasConceptScore W2034705058C2816523 @default.
• W2034705058 hasConceptScore W2034705058C29941650 @default.
• W2034705058 hasConceptScore W2034705058C39432304 @default.
• W2034705058 hasConceptScore W2034705058C65589250 @default.
• W2034705058 hasConceptScore W2034705058C87717796 @default.
• W2034705058 hasIssue "B10" @default.

• next