FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1952842796> ?p ?o ?g. }

• W1952842796 endingPage "n/a" @default.
• W1952842796 startingPage "n/a" @default.
• W1952842796 abstract "[1] In paper 1 we described a methodology to model coupled fluid flow and deformation in composite salt and siliciclastic tectonic systems and investigated their compaction and overpressuring behavior prior to and during continental margin-scale gravitational spreading. Compaction-driven Darcy fluid flow in clastic sediments is coupled through the effective pressure to their frictional-plastic yield and mechanical deformation. Viscous flow of the underlying salt is independent of fluid pressure. Paper 1 presented prototype models that are limited to single uniform sediment lithologies, either sandstone-type or shale-type, that undergo mechanical and volumetric viscous compaction. In this paper we present models with layered sandstone-type and shale-type lithologies designed to better approximate the more complex stratigraphy of the Gulf of Mexico, our natural example. A first set of models demonstrates that layered lithologies can produce fluid pressure regimes similar to those observed in sedimentary basins. We then introduce an improved formulation of viscous compaction that includes a stronger dependence on porosity and depth (used as proxy for temperature), thereby more effectively self-limiting viscous compaction. A second set of models with the improved viscous compaction formulation demonstrates that the onset of gravity spreading is mainly controlled by overpressuring in the landward end of the salt basin and that resulting shortening in the distal part is partly accommodated by horizontal compaction. Models with moderately high fluid pressure best reproduce conditions considered to have been necessary for large-scale gravitational spreading in the northwestern Gulf of Mexico, which led to the formation of the Perdido Fold Belt." @default.
• W1952842796 created "2016-06-24" @default.
• W1952842796 creator A5029218873 @default.
• W1952842796 creator A5051880517 @default.
• W1952842796 date "2012-07-26" @default.
• W1952842796 modified "2023-09-26" @default.
• W1952842796 title "Coupled fluid flow and sediment deformation in margin-scale salt-tectonic systems: 2. Layered sediment models and application to the northwestern Gulf of Mexico" @default.
• W1952842796 cites W1509405854 @default.
• W1952842796 cites W1577210620 @default.
• W1952842796 cites W1667665679 @default.
• W1952842796 cites W1971167665 @default.
• W1952842796 cites W1973501867 @default.
• W1952842796 cites W1982816080 @default.
• W1952842796 cites W1994763452 @default.
• W1952842796 cites W1996938749 @default.
• W1952842796 cites W1999647229 @default.
• W1952842796 cites W2004482114 @default.
• W1952842796 cites W2007728421 @default.
• W1952842796 cites W2013719700 @default.
• W1952842796 cites W2029730606 @default.
• W1952842796 cites W2040046495 @default.
• W1952842796 cites W2049124682 @default.
• W1952842796 cites W2058430476 @default.
• W1952842796 cites W2062024970 @default.
• W1952842796 cites W2064619444 @default.
• W1952842796 cites W2071067390 @default.
• W1952842796 cites W2083603261 @default.
• W1952842796 cites W2084107403 @default.
• W1952842796 cites W2091893951 @default.
• W1952842796 cites W2094488484 @default.
• W1952842796 cites W2094675334 @default.
• W1952842796 cites W2102010978 @default.
• W1952842796 cites W2119205759 @default.
• W1952842796 cites W2122189928 @default.
• W1952842796 cites W2126035186 @default.
• W1952842796 cites W2134946466 @default.
• W1952842796 cites W2137625220 @default.
• W1952842796 cites W2154463579 @default.
• W1952842796 cites W2169147816 @default.
• W1952842796 cites W2169973427 @default.
• W1952842796 cites W2487040690 @default.
• W1952842796 cites W2500818495 @default.
• W1952842796 cites W2724477917 @default.
• W1952842796 cites W2793684479 @default.
• W1952842796 cites W4230993336 @default.
• W1952842796 cites W4245743681 @default.
• W1952842796 cites W4249005320 @default.
• W1952842796 doi "https://doi.org/10.1029/2011tc003035" @default.
• W1952842796 hasPublicationYear "2012" @default.
• W1952842796 type Work @default.
• W1952842796 sameAs 1952842796 @default.
• W1952842796 citedByCount "9" @default.
• W1952842796 countsByYear W19528427962013 @default.
• W1952842796 countsByYear W19528427962014 @default.
• W1952842796 countsByYear W19528427962016 @default.
• W1952842796 countsByYear W19528427962017 @default.
• W1952842796 countsByYear W19528427962018 @default.
• W1952842796 countsByYear W19528427962021 @default.
• W1952842796 crossrefType "journal-article" @default.
• W1952842796 hasAuthorship W1952842796A5029218873 @default.
• W1952842796 hasAuthorship W1952842796A5051880517 @default.
• W1952842796 hasBestOaLocation W19528427961 @default.
• W1952842796 hasConcept C114793014 @default.
• W1952842796 hasConcept C122792734 @default.
• W1952842796 hasConcept C127313418 @default.
• W1952842796 hasConcept C17409809 @default.
• W1952842796 hasConcept C187320778 @default.
• W1952842796 hasConcept C196715460 @default.
• W1952842796 hasConcept C5900021 @default.
• W1952842796 hasConcept C6494504 @default.
• W1952842796 hasConceptScore W1952842796C114793014 @default.
• W1952842796 hasConceptScore W1952842796C122792734 @default.
• W1952842796 hasConceptScore W1952842796C127313418 @default.
• W1952842796 hasConceptScore W1952842796C17409809 @default.
• W1952842796 hasConceptScore W1952842796C187320778 @default.
• W1952842796 hasConceptScore W1952842796C196715460 @default.
• W1952842796 hasConceptScore W1952842796C5900021 @default.
• W1952842796 hasConceptScore W1952842796C6494504 @default.
• W1952842796 hasIssue "4" @default.
• W1952842796 hasLocation W19528427961 @default.
• W1952842796 hasOpenAccess W1952842796 @default.
• W1952842796 hasPrimaryLocation W19528427961 @default.
• W1952842796 hasRelatedWork W1793231925 @default.
• W1952842796 hasRelatedWork W1979607177 @default.
• W1952842796 hasRelatedWork W2219155975 @default.
• W1952842796 hasRelatedWork W2353207713 @default.
• W1952842796 hasRelatedWork W2355623062 @default.
• W1952842796 hasRelatedWork W2371302029 @default.
• W1952842796 hasRelatedWork W2378348218 @default.
• W1952842796 hasRelatedWork W2385579777 @default.
• W1952842796 hasRelatedWork W2386590832 @default.
• W1952842796 hasRelatedWork W2393520445 @default.
• W1952842796 hasVolume "31" @default.
• W1952842796 isParatext "false" @default.
• W1952842796 isRetracted "false" @default.
• W1952842796 magId "1952842796" @default.
• W1952842796 workType "article" @default.