FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2072904001> ?p ?o ?g. }

• W2072904001 endingPage "3215" @default.
• W2072904001 startingPage "3205" @default.
• W2072904001 abstract "Some low‐chloride pore waters observed in accretionary complexes are thought to result from clay dehydration and subsequent migration of the released water along faults or sand layers. We test this hypothesis with a two‐dimensional flow and transport model for a cross section of the northern Barbados accretionary complex. The model flow system is driven by consolidation of the accreted sediments and by fluids from smectite clay dehydration. Steady state simulations result in concentrations that are too high along the décollement fault and too low near the seafloor. In a transient model we simulate buildup and release of fluids by assuming that strain or hydrofracture along the fault causes an instantaneous increase in décollement permeability of 2–3 orders of magnitude. With such an increase, the observed concentrations can be achieved in 100–1000 years. Also pressures along the fault rise to near lithostatic values in 10–100 years and remain high for 1000–10,000 years. This pressure rise may represent a mechanism for sustaining high fault permeabilities long after the initial increase." @default.
• W2072904001 created "2016-06-24" @default.
• W2072904001 creator A5053558713 @default.
• W2072904001 creator A5082234767 @default.
• W2072904001 creator A5087476360 @default.
• W2072904001 date "1995-12-01" @default.
• W2072904001 modified "2023-10-14" @default.
• W2072904001 title "Episodic and constant flow models for the origin of low‐chloride waters in a modern accretionary complex" @default.
• W2072904001 cites W1971534802 @default.
• W2072904001 cites W1987908336 @default.
• W2072904001 cites W2003550312 @default.
• W2072904001 cites W2006270629 @default.
• W2072904001 cites W2009316828 @default.
• W2072904001 cites W2021714816 @default.
• W2072904001 cites W2024485649 @default.
• W2072904001 cites W2026889131 @default.
• W2072904001 cites W2030265085 @default.
• W2072904001 cites W2034032223 @default.
• W2072904001 cites W2036017192 @default.
• W2072904001 cites W2046166697 @default.
• W2072904001 cites W2060390546 @default.
• W2072904001 cites W2072741523 @default.
• W2072904001 cites W2076803851 @default.
• W2072904001 cites W2077804311 @default.
• W2072904001 cites W2089614630 @default.
• W2072904001 cites W2089973955 @default.
• W2072904001 cites W2093114365 @default.
• W2072904001 cites W2107414840 @default.
• W2072904001 cites W2117818056 @default.
• W2072904001 cites W2125843303 @default.
• W2072904001 cites W2126603647 @default.
• W2072904001 cites W2134946466 @default.
• W2072904001 cites W2140606492 @default.
• W2072904001 cites W2154880694 @default.
• W2072904001 cites W2164781010 @default.
• W2072904001 cites W2182388070 @default.
• W2072904001 cites W2313488100 @default.
• W2072904001 cites W4362212951 @default.
• W2072904001 doi "https://doi.org/10.1029/95wr02569" @default.
• W2072904001 hasPublicationYear "1995" @default.
• W2072904001 type Work @default.
• W2072904001 sameAs 2072904001 @default.
• W2072904001 citedByCount "122" @default.
• W2072904001 countsByYear W20729040012012 @default.
• W2072904001 countsByYear W20729040012013 @default.
• W2072904001 countsByYear W20729040012014 @default.
• W2072904001 countsByYear W20729040012015 @default.
• W2072904001 countsByYear W20729040012016 @default.
• W2072904001 countsByYear W20729040012017 @default.
• W2072904001 countsByYear W20729040012018 @default.
• W2072904001 countsByYear W20729040012019 @default.
• W2072904001 countsByYear W20729040012020 @default.
• W2072904001 countsByYear W20729040012021 @default.
• W2072904001 countsByYear W20729040012023 @default.
• W2072904001 crossrefType "journal-article" @default.
• W2072904001 hasAuthorship W2072904001A5053558713 @default.
• W2072904001 hasAuthorship W2072904001A5082234767 @default.
• W2072904001 hasAuthorship W2072904001A5087476360 @default.
• W2072904001 hasConcept C102579867 @default.
• W2072904001 hasConcept C114793014 @default.
• W2072904001 hasConcept C117485682 @default.
• W2072904001 hasConcept C120882062 @default.
• W2072904001 hasConcept C121955636 @default.
• W2072904001 hasConcept C127313418 @default.
• W2072904001 hasConcept C144133560 @default.
• W2072904001 hasConcept C165205528 @default.
• W2072904001 hasConcept C175551986 @default.
• W2072904001 hasConcept C185592680 @default.
• W2072904001 hasConcept C187320778 @default.
• W2072904001 hasConcept C191897082 @default.
• W2072904001 hasConcept C192562407 @default.
• W2072904001 hasConcept C199289684 @default.
• W2072904001 hasConcept C2776014549 @default.
• W2072904001 hasConcept C2778695967 @default.
• W2072904001 hasConcept C2778769901 @default.
• W2072904001 hasConcept C41625074 @default.
• W2072904001 hasConcept C44140439 @default.
• W2072904001 hasConcept C55493867 @default.
• W2072904001 hasConcept C58097730 @default.
• W2072904001 hasConcept C5900021 @default.
• W2072904001 hasConcept C77928131 @default.
• W2072904001 hasConcept C8058405 @default.
• W2072904001 hasConcept C80781247 @default.
• W2072904001 hasConceptScore W2072904001C102579867 @default.
• W2072904001 hasConceptScore W2072904001C114793014 @default.
• W2072904001 hasConceptScore W2072904001C117485682 @default.
• W2072904001 hasConceptScore W2072904001C120882062 @default.
• W2072904001 hasConceptScore W2072904001C121955636 @default.
• W2072904001 hasConceptScore W2072904001C127313418 @default.
• W2072904001 hasConceptScore W2072904001C144133560 @default.
• W2072904001 hasConceptScore W2072904001C165205528 @default.
• W2072904001 hasConceptScore W2072904001C175551986 @default.
• W2072904001 hasConceptScore W2072904001C185592680 @default.
• W2072904001 hasConceptScore W2072904001C187320778 @default.
• W2072904001 hasConceptScore W2072904001C191897082 @default.
• W2072904001 hasConceptScore W2072904001C192562407 @default.
• W2072904001 hasConceptScore W2072904001C199289684 @default.
• W2072904001 hasConceptScore W2072904001C2776014549 @default.

• next