FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022174581> ?p ?o ?g. }

• W2022174581 endingPage "1483" @default.
• W2022174581 startingPage "1452" @default.
• W2022174581 abstract "Abstract Distributary channel systems are an important component of deltaic systems, but details of their branching pattern, stream‐order, internal variability and relation with adjacent levée, bay and bayhead delta are rather poorly documented in ancient examples. Photomosaic and measured sections collected along a gooseneck‐shaped canyon in southern Utah allow direct mapping of the branching pattern of an ancient distributary system. The main channel belt is ca 250 m wide and narrows to ca 200 m downstream of the branching point. A subordinate channel belt, ca 80 m wide, branches off of the main channel, forming a distinctly asymmetrical branching pattern. Water discharge in the main channel is estimated to be 85 to 170 m 3 sec −1 . Comparison with palaeodischarge estimates of trunk rivers mapped in previous studies suggests that the branching documented in this study probably is a fourth‐order split. The distributary channels are characterized by a U‐shaped geometry filled with medium‐grained, cross‐bedded sandstone, and are dominated by lateral accretion, suggesting limited lateral migration and moderate sinuosity. Tidally influenced facies and limited trace fossils indicate direct marine influence. The distributary channels erode into adjacent levée and underlying heterolithic bay‐fill deposits, and the marine influence suggests that they were deposited on a lower delta plain, rather than on a non‐marine floodplain. The subordinate channel fed a bayhead delta, suggesting that it was formed by a partial avulsion, rather than bifurcation around a mouth bar, as is more characteristic of terminal distributary channels. Channel‐floor drapes, bar‐accretion drapes and abandoned channel fills within the sandstone channel belts represent the most important heterogeneity from the perspective of reservoir characterization." @default.
• W2022174581 created "2016-06-24" @default.
• W2022174581 creator A5023578647 @default.
• W2022174581 creator A5089206039 @default.
• W2022174581 date "2014-03-21" @default.
• W2022174581 modified "2023-10-01" @default.
• W2022174581 title "Facies architecture of asymmetrical branching distributary channels: Cretaceous Ferron Sandstone, Utah, USA" @default.
• W2022174581 cites W1564757458 @default.
• W2022174581 cites W1579610342 @default.
• W2022174581 cites W1662857152 @default.
• W2022174581 cites W1751425781 @default.
• W2022174581 cites W1968313731 @default.
• W2022174581 cites W1975778409 @default.
• W2022174581 cites W2012887763 @default.
• W2022174581 cites W2014268565 @default.
• W2022174581 cites W2023036480 @default.
• W2022174581 cites W2053906134 @default.
• W2022174581 cites W2057184487 @default.
• W2022174581 cites W2057962730 @default.
• W2022174581 cites W2059950589 @default.
• W2022174581 cites W2098418938 @default.
• W2022174581 cites W2099512080 @default.
• W2022174581 cites W2100067434 @default.
• W2022174581 cites W2101236769 @default.
• W2022174581 cites W2102752950 @default.
• W2022174581 cites W2110536870 @default.
• W2022174581 cites W2113298788 @default.
• W2022174581 cites W2123965421 @default.
• W2022174581 cites W2132272817 @default.
• W2022174581 cites W2138504595 @default.
• W2022174581 cites W2138666479 @default.
• W2022174581 cites W2139703970 @default.
• W2022174581 cites W2139920049 @default.
• W2022174581 cites W2146063783 @default.
• W2022174581 cites W2147820481 @default.
• W2022174581 cites W2168262750 @default.
• W2022174581 cites W2216559411 @default.
• W2022174581 cites W2249170896 @default.
• W2022174581 cites W4246500580 @default.
• W2022174581 doi "https://doi.org/10.1111/sed.12104" @default.
• W2022174581 hasPublicationYear "2014" @default.
• W2022174581 type Work @default.
• W2022174581 sameAs 2022174581 @default.
• W2022174581 citedByCount "16" @default.
• W2022174581 countsByYear W20221745812015 @default.
• W2022174581 countsByYear W20221745812016 @default.
• W2022174581 countsByYear W20221745812017 @default.
• W2022174581 countsByYear W20221745812018 @default.
• W2022174581 countsByYear W20221745812019 @default.
• W2022174581 countsByYear W20221745812020 @default.
• W2022174581 countsByYear W20221745812021 @default.
• W2022174581 countsByYear W20221745812022 @default.
• W2022174581 crossrefType "journal-article" @default.
• W2022174581 hasAuthorship W2022174581A5023578647 @default.
• W2022174581 hasAuthorship W2022174581A5089206039 @default.
• W2022174581 hasConcept C109007969 @default.
• W2022174581 hasConcept C114793014 @default.
• W2022174581 hasConcept C12294951 @default.
• W2022174581 hasConcept C127313418 @default.
• W2022174581 hasConcept C127413603 @default.
• W2022174581 hasConcept C134872888 @default.
• W2022174581 hasConcept C146588470 @default.
• W2022174581 hasConcept C146978453 @default.
• W2022174581 hasConcept C151730666 @default.
• W2022174581 hasConcept C2779905724 @default.
• W2022174581 hasConcept C2780589035 @default.
• W2022174581 hasConcept C5072461 @default.
• W2022174581 hasConceptScore W2022174581C109007969 @default.
• W2022174581 hasConceptScore W2022174581C114793014 @default.
• W2022174581 hasConceptScore W2022174581C12294951 @default.
• W2022174581 hasConceptScore W2022174581C127313418 @default.
• W2022174581 hasConceptScore W2022174581C127413603 @default.
• W2022174581 hasConceptScore W2022174581C134872888 @default.
• W2022174581 hasConceptScore W2022174581C146588470 @default.
• W2022174581 hasConceptScore W2022174581C146978453 @default.
• W2022174581 hasConceptScore W2022174581C151730666 @default.
• W2022174581 hasConceptScore W2022174581C2779905724 @default.
• W2022174581 hasConceptScore W2022174581C2780589035 @default.
• W2022174581 hasConceptScore W2022174581C5072461 @default.
• W2022174581 hasIssue "5" @default.
• W2022174581 hasLocation W20221745811 @default.
• W2022174581 hasOpenAccess W2022174581 @default.
• W2022174581 hasPrimaryLocation W20221745811 @default.
• W2022174581 hasRelatedWork W1981323548 @default.
• W2022174581 hasRelatedWork W1985727369 @default.
• W2022174581 hasRelatedWork W1996737738 @default.
• W2022174581 hasRelatedWork W2053157878 @default.
• W2022174581 hasRelatedWork W2062696754 @default.
• W2022174581 hasRelatedWork W2361989743 @default.
• W2022174581 hasRelatedWork W2376157092 @default.
• W2022174581 hasRelatedWork W2380332148 @default.
• W2022174581 hasRelatedWork W2380959899 @default.
• W2022174581 hasRelatedWork W2958184617 @default.
• W2022174581 hasVolume "61" @default.
• W2022174581 isParatext "false" @default.
• W2022174581 isRetracted "false" @default.
• W2022174581 magId "2022174581" @default.
• W2022174581 workType "article" @default.