FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2032053568> ?p ?o ?g. }

• W2032053568 endingPage "20" @default.
• W2032053568 startingPage "11" @default.
• W2032053568 abstract "Abstract In mudstones of the Ursa Basin, Gulf of Mexico, the volume of voids to solids, or void ratio, ranges from 4 (porosity = 80%) at the seafloor to 0.6 (porosity = 37%) at 600 m below seafloor. This seven-fold change in void ratio can only be described by a compaction model that includes greater sediment stiffening with stress than has commonly been used in geotechnical or geological approaches. Through uniaxial consolidation experiments, we show that specific volume (v = 1 + void ratio) declines as an exponential function of effective stress. We use this relationship to successfully predict in-situ overpressures at Integrated Ocean Drilling Program (IODP) Sites U1322 and U1324. This technique can be used around the world to describe sediment compaction and predict pore pressure in the first 1000 m below seafloor. Rapid sediment consolidation near the seafloor provides the fluid source that generates overpressure despite the fact that these sediments have high permeability. Ultimately sediment consolidation is a first order control on when and at what depth overpressure will be generated in the subsurface. This in turn will impact whether submarine landslides are expected and the regional gradient of continental margins." @default.
• W2032053568 created "2016-06-24" @default.
• W2032053568 creator A5008198868 @default.
• W2032053568 creator A5020440897 @default.
• W2032053568 creator A5040844094 @default.
• W2032053568 creator A5080184496 @default.
• W2032053568 date "2011-05-01" @default.
• W2032053568 modified "2023-10-16" @default.
• W2032053568 title "Consolidation and overpressure near the seafloor in the Ursa Basin, Deepwater Gulf of Mexico" @default.
• W2032053568 cites W1964306993 @default.
• W2032053568 cites W1970530701 @default.
• W2032053568 cites W1998921845 @default.
• W2032053568 cites W2000008856 @default.
• W2032053568 cites W2004482114 @default.
• W2032053568 cites W2013593297 @default.
• W2032053568 cites W2016207804 @default.
• W2032053568 cites W2039296642 @default.
• W2032053568 cites W2040511246 @default.
• W2032053568 cites W2041326290 @default.
• W2032053568 cites W2047898003 @default.
• W2032053568 cites W2048572409 @default.
• W2032053568 cites W2066309818 @default.
• W2032053568 cites W2069769449 @default.
• W2032053568 cites W2075147434 @default.
• W2032053568 cites W2076638194 @default.
• W2032053568 cites W2077528177 @default.
• W2032053568 cites W2103433309 @default.
• W2032053568 cites W2112558023 @default.
• W2032053568 cites W2134010836 @default.
• W2032053568 cites W2139641685 @default.
• W2032053568 cites W2148628311 @default.
• W2032053568 cites W2153438067 @default.
• W2032053568 cites W2159181111 @default.
• W2032053568 cites W2159778482 @default.
• W2032053568 cites W2588373281 @default.
• W2032053568 doi "https://doi.org/10.1016/j.epsl.2011.02.007" @default.
• W2032053568 hasPublicationYear "2011" @default.
• W2032053568 type Work @default.
• W2032053568 sameAs 2032053568 @default.
• W2032053568 citedByCount "53" @default.
• W2032053568 countsByYear W20320535682012 @default.
• W2032053568 countsByYear W20320535682013 @default.
• W2032053568 countsByYear W20320535682014 @default.
• W2032053568 countsByYear W20320535682015 @default.
• W2032053568 countsByYear W20320535682016 @default.
• W2032053568 countsByYear W20320535682017 @default.
• W2032053568 countsByYear W20320535682018 @default.
• W2032053568 countsByYear W20320535682019 @default.
• W2032053568 countsByYear W20320535682020 @default.
• W2032053568 countsByYear W20320535682021 @default.
• W2032053568 countsByYear W20320535682022 @default.
• W2032053568 countsByYear W20320535682023 @default.
• W2032053568 crossrefType "journal-article" @default.
• W2032053568 hasAuthorship W2032053568A5008198868 @default.
• W2032053568 hasAuthorship W2032053568A5020440897 @default.
• W2032053568 hasAuthorship W2032053568A5040844094 @default.
• W2032053568 hasAuthorship W2032053568A5080184496 @default.
• W2032053568 hasConcept C109007969 @default.
• W2032053568 hasConcept C111368507 @default.
• W2032053568 hasConcept C114793014 @default.
• W2032053568 hasConcept C117485682 @default.
• W2032053568 hasConcept C121332964 @default.
• W2032053568 hasConcept C121955636 @default.
• W2032053568 hasConcept C127313418 @default.
• W2032053568 hasConcept C144133560 @default.
• W2032053568 hasConcept C165205528 @default.
• W2032053568 hasConcept C2776014549 @default.
• W2032053568 hasConcept C29452850 @default.
• W2032053568 hasConcept C97355855 @default.
• W2032053568 hasConceptScore W2032053568C109007969 @default.
• W2032053568 hasConceptScore W2032053568C111368507 @default.
• W2032053568 hasConceptScore W2032053568C114793014 @default.
• W2032053568 hasConceptScore W2032053568C117485682 @default.
• W2032053568 hasConceptScore W2032053568C121332964 @default.
• W2032053568 hasConceptScore W2032053568C121955636 @default.
• W2032053568 hasConceptScore W2032053568C127313418 @default.
• W2032053568 hasConceptScore W2032053568C144133560 @default.
• W2032053568 hasConceptScore W2032053568C165205528 @default.
• W2032053568 hasConceptScore W2032053568C2776014549 @default.
• W2032053568 hasConceptScore W2032053568C29452850 @default.
• W2032053568 hasConceptScore W2032053568C97355855 @default.
• W2032053568 hasIssue "1-2" @default.
• W2032053568 hasLocation W20320535681 @default.
• W2032053568 hasOpenAccess W2032053568 @default.
• W2032053568 hasPrimaryLocation W20320535681 @default.
• W2032053568 hasRelatedWork W2150459800 @default.
• W2032053568 hasRelatedWork W2604251004 @default.
• W2032053568 hasRelatedWork W2973786500 @default.
• W2032053568 hasRelatedWork W3016255354 @default.
• W2032053568 hasRelatedWork W3087925122 @default.
• W2032053568 hasRelatedWork W3184396329 @default.
• W2032053568 hasRelatedWork W36978812 @default.
• W2032053568 hasRelatedWork W4220837764 @default.
• W2032053568 hasRelatedWork W4281741018 @default.
• W2032053568 hasRelatedWork W4283708435 @default.
• W2032053568 hasVolume "305" @default.
• W2032053568 isParatext "false" @default.
• W2032053568 isRetracted "false" @default.

• next