FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2090114189> ?p ?o ?g. }

• W2090114189 abstract "Pressure solution is widely regarded as a mechanism of ductile deformation in the upper crust. It is driven by stress differences and its rate is affected by temperature, grain size, and fluid chemistry. Pressure solution involves dissolution at grain contacts under high stress and precipitation at grain contacts on pore surfaces under low stress, leading to porosity reduction by precipitation in the pore space or by grain indentation. For a system closed at a grain scale, pressure solution is traditionally described by a mechanism involving three steps: (1) dissolution at intergranular interfaces, (2) diffusion of solutes inside the contact between two grains, and (3) precipitation on the surface of the grains in contact with the pore fluid. In this paper we propose a model where we have added a fourth step to this process, diffusive transport to other open pores, to account for the macroscopic diffusion of solutes in pore fluids, such that the deformation is not closed at the grain scale. In this model, differences in mineral solubility due to variations in stress and grain size produce concentration gradients which drive diffusive mass transport. The interaction between pressure solution at a grain scale and transport over distances of several grains can lead to the amplification of initial porosity heterogeneities and subsequent localization of deformation. Regions of intense dissolution compact and form “bands” in close proximity to regions where the porosity reduction is mainly due to cementation. Pressure solution augmented by large‐scale diffusional transport will cause mass transport from fine‐grained to coarse‐grained rock volumes. We show that such processes are important during both diagenesis of sediments and compaction of fault gouge." @default.
• W2090114189 created "2016-06-24" @default.
• W2090114189 creator A5023503396 @default.
• W2090114189 creator A5037742614 @default.
• W2090114189 creator A5043344418 @default.
• W2090114189 creator A5049442180 @default.
• W2090114189 creator A5060612130 @default.
• W2090114189 date "2002-11-01" @default.
• W2090114189 modified "2023-10-18" @default.
• W2090114189 title "Coupling between pressure solution creep and diffusive mass transport in porous rocks" @default.
• W2090114189 cites W1552158845 @default.
• W2090114189 cites W1581621688 @default.
• W2090114189 cites W1592669541 @default.
• W2090114189 cites W1667665679 @default.
• W2090114189 cites W1964751056 @default.
• W2090114189 cites W1968047999 @default.
• W2090114189 cites W1969635208 @default.
• W2090114189 cites W1970790326 @default.
• W2090114189 cites W1973087299 @default.
• W2090114189 cites W1975717988 @default.
• W2090114189 cites W1985485429 @default.
• W2090114189 cites W1988005274 @default.
• W2090114189 cites W1996284022 @default.
• W2090114189 cites W1999647229 @default.
• W2090114189 cites W2001486179 @default.
• W2090114189 cites W2006785189 @default.
• W2090114189 cites W2010292438 @default.
• W2090114189 cites W2011211424 @default.
• W2090114189 cites W2011307050 @default.
• W2090114189 cites W2019995870 @default.
• W2090114189 cites W2024972495 @default.
• W2090114189 cites W2029713417 @default.
• W2090114189 cites W2046660116 @default.
• W2090114189 cites W2047533256 @default.
• W2090114189 cites W2053997518 @default.
• W2090114189 cites W2056301165 @default.
• W2090114189 cites W2063555355 @default.
• W2090114189 cites W2064597130 @default.
• W2090114189 cites W2066838818 @default.
• W2090114189 cites W2069311979 @default.
• W2090114189 cites W2069923477 @default.
• W2090114189 cites W2071067390 @default.
• W2090114189 cites W2081882231 @default.
• W2090114189 cites W2081923176 @default.
• W2090114189 cites W2082995413 @default.
• W2090114189 cites W2088233368 @default.
• W2090114189 cites W2092197672 @default.
• W2090114189 cites W2115760436 @default.
• W2090114189 cites W2124352753 @default.
• W2090114189 cites W2128136955 @default.
• W2090114189 cites W2139242345 @default.
• W2090114189 cites W2162473845 @default.
• W2090114189 cites W2168649638 @default.
• W2090114189 cites W2170102073 @default.
• W2090114189 cites W2332356198 @default.
• W2090114189 cites W4206154619 @default.
• W2090114189 cites W4233497874 @default.
• W2090114189 cites W4251759016 @default.
• W2090114189 cites W4255965168 @default.
• W2090114189 cites W4383613990 @default.
• W2090114189 doi "https://doi.org/10.1029/2001jb000287" @default.
• W2090114189 hasPublicationYear "2002" @default.
• W2090114189 type Work @default.
• W2090114189 sameAs 2090114189 @default.
• W2090114189 citedByCount "60" @default.
• W2090114189 countsByYear W20901141892012 @default.
• W2090114189 countsByYear W20901141892013 @default.
• W2090114189 countsByYear W20901141892014 @default.
• W2090114189 countsByYear W20901141892016 @default.
• W2090114189 countsByYear W20901141892017 @default.
• W2090114189 countsByYear W20901141892018 @default.
• W2090114189 countsByYear W20901141892019 @default.
• W2090114189 countsByYear W20901141892020 @default.
• W2090114189 countsByYear W20901141892021 @default.
• W2090114189 countsByYear W20901141892022 @default.
• W2090114189 countsByYear W20901141892023 @default.
• W2090114189 crossrefType "journal-article" @default.
• W2090114189 hasAuthorship W2090114189A5023503396 @default.
• W2090114189 hasAuthorship W2090114189A5037742614 @default.
• W2090114189 hasAuthorship W2090114189A5043344418 @default.
• W2090114189 hasAuthorship W2090114189A5049442180 @default.
• W2090114189 hasAuthorship W2090114189A5060612130 @default.
• W2090114189 hasBestOaLocation W20901141891 @default.
• W2090114189 hasConcept C107054158 @default.
• W2090114189 hasConcept C121332964 @default.
• W2090114189 hasConcept C127313418 @default.
• W2090114189 hasConcept C127413603 @default.
• W2090114189 hasConcept C138885662 @default.
• W2090114189 hasConcept C149912024 @default.
• W2090114189 hasConcept C153294291 @default.
• W2090114189 hasConcept C159985019 @default.
• W2090114189 hasConcept C174178034 @default.
• W2090114189 hasConcept C192191005 @default.
• W2090114189 hasConcept C192562407 @default.
• W2090114189 hasConcept C199289684 @default.
• W2090114189 hasConcept C21036866 @default.
• W2090114189 hasConcept C41895202 @default.
• W2090114189 hasConcept C42360764 @default.
• W2090114189 hasConcept C47908070 @default.
• W2090114189 hasConcept C6648577 @default.

• next