Matches in SemOpenAlex for { <https://semopenalex.org/work/W2128314497> ?p ?o ?g. }
- W2128314497 endingPage "836" @default.
- W2128314497 startingPage "825" @default.
- W2128314497 abstract "Constraining the depositional gradient of ancient alluvial river systems can aid in reconstructing landscapes and estimating paleodischarge by establishing boundaries on the climatic and tectonic history of continental sequences. We present three methods for estimating ancient depositional gradients based on the interpreted mode of sediment transport for the range of particle sizes found on the beds of modern rivers or preserved in channel fills. For sandy rivers with suspension as the dominant mode of sediment transport, these methods take advantage of observations that can be directly obtained from preserved strata, including measurements of paleo flow depth and grain size. The first method relates river slope to Shields number at bankfull flow. The second method is similar to the first but allows for variation in Shields number at bankfull flow with grain diameter. The final method relies on criteria required for both suspended- and bed-material load sediment transport in the same system and is the most comprehensive and physically justified method. We present each method and test them with modern river datasets to verify accuracy and help constrain uncertainty—the first step to adapting them to ancient systems. Results indicate that all methods estimate slope within a factor of two. These methods are potentially very powerful for interpreting sandy fluvial deposits because they can provide reasonably accurate quantitative estimates of paleoslope, an elusive yet important environmental variable." @default.
- W2128314497 created "2016-06-24" @default.
- W2128314497 creator A5024009329 @default.
- W2128314497 creator A5059668888 @default.
- W2128314497 creator A5066540096 @default.
- W2128314497 creator A5077318979 @default.
- W2128314497 date "2014-10-08" @default.
- W2128314497 modified "2023-10-18" @default.
- W2128314497 title "Paleoslope Reconstruction In Sandy Suspended-Load-Dominant Rivers" @default.
- W2128314497 cites W144886082 @default.
- W2128314497 cites W1528850606 @default.
- W2128314497 cites W1551957387 @default.
- W2128314497 cites W1575915308 @default.
- W2128314497 cites W1577071438 @default.
- W2128314497 cites W1581618764 @default.
- W2128314497 cites W1586826975 @default.
- W2128314497 cites W1629642785 @default.
- W2128314497 cites W1965472552 @default.
- W2128314497 cites W1973272074 @default.
- W2128314497 cites W1973408638 @default.
- W2128314497 cites W1974743957 @default.
- W2128314497 cites W1979321080 @default.
- W2128314497 cites W1981712236 @default.
- W2128314497 cites W1991129484 @default.
- W2128314497 cites W1992030132 @default.
- W2128314497 cites W1995040253 @default.
- W2128314497 cites W1996720026 @default.
- W2128314497 cites W2004729062 @default.
- W2128314497 cites W2006265565 @default.
- W2128314497 cites W2018319064 @default.
- W2128314497 cites W2026085067 @default.
- W2128314497 cites W2051927174 @default.
- W2128314497 cites W2053906134 @default.
- W2128314497 cites W2063401060 @default.
- W2128314497 cites W2068724623 @default.
- W2128314497 cites W2069320488 @default.
- W2128314497 cites W2073713430 @default.
- W2128314497 cites W2113929468 @default.
- W2128314497 cites W2121081932 @default.
- W2128314497 cites W2124595812 @default.
- W2128314497 cites W2129680599 @default.
- W2128314497 cites W2130650877 @default.
- W2128314497 cites W2135130717 @default.
- W2128314497 cites W2136951817 @default.
- W2128314497 cites W2138666479 @default.
- W2128314497 cites W2140747300 @default.
- W2128314497 cites W2151182374 @default.
- W2128314497 cites W2151880780 @default.
- W2128314497 cites W2156206800 @default.
- W2128314497 cites W2166184284 @default.
- W2128314497 cites W2166930832 @default.
- W2128314497 cites W2167952974 @default.
- W2128314497 cites W2286349128 @default.
- W2128314497 cites W2305168329 @default.
- W2128314497 cites W2342931149 @default.
- W2128314497 cites W2343694057 @default.
- W2128314497 cites W2486618570 @default.
- W2128314497 cites W2504329849 @default.
- W2128314497 cites W2616344388 @default.
- W2128314497 cites W3125932593 @default.
- W2128314497 cites W333275647 @default.
- W2128314497 cites W93135601 @default.
- W2128314497 doi "https://doi.org/10.2110/jsr.2014.60" @default.
- W2128314497 hasPublicationYear "2014" @default.
- W2128314497 type Work @default.
- W2128314497 sameAs 2128314497 @default.
- W2128314497 citedByCount "29" @default.
- W2128314497 countsByYear W21283144972016 @default.
- W2128314497 countsByYear W21283144972017 @default.
- W2128314497 countsByYear W21283144972018 @default.
- W2128314497 countsByYear W21283144972019 @default.
- W2128314497 countsByYear W21283144972020 @default.
- W2128314497 countsByYear W21283144972021 @default.
- W2128314497 countsByYear W21283144972022 @default.
- W2128314497 countsByYear W21283144972023 @default.
- W2128314497 crossrefType "journal-article" @default.
- W2128314497 hasAuthorship W2128314497A5024009329 @default.
- W2128314497 hasAuthorship W2128314497A5059668888 @default.
- W2128314497 hasAuthorship W2128314497A5066540096 @default.
- W2128314497 hasAuthorship W2128314497A5077318979 @default.
- W2128314497 hasConcept C114793014 @default.
- W2128314497 hasConcept C127313418 @default.
- W2128314497 hasConcept C187320778 @default.
- W2128314497 hasConcept C76886044 @default.
- W2128314497 hasConceptScore W2128314497C114793014 @default.
- W2128314497 hasConceptScore W2128314497C127313418 @default.
- W2128314497 hasConceptScore W2128314497C187320778 @default.
- W2128314497 hasConceptScore W2128314497C76886044 @default.
- W2128314497 hasIssue "10" @default.
- W2128314497 hasLocation W21283144971 @default.
- W2128314497 hasOpenAccess W2128314497 @default.
- W2128314497 hasPrimaryLocation W21283144971 @default.
- W2128314497 hasRelatedWork W1652433593 @default.
- W2128314497 hasRelatedWork W2008590108 @default.
- W2128314497 hasRelatedWork W2014633439 @default.
- W2128314497 hasRelatedWork W2020535921 @default.
- W2128314497 hasRelatedWork W2077938109 @default.
- W2128314497 hasRelatedWork W2090030785 @default.