{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1363670318846375552.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1144/gsjgs.140.5.0725"}},{"identifier":{"@type":"URI","@value":"https://www.lyellcollection.org/doi/pdf/10.1144/gsjgs.140.5.0725"}},{"identifier":{"@type":"NAID","@value":"30031598338"}}],"dc:title":[{"@value":"Pressure solution in nature, theory and experiment"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Some of the features of water enhanced deformation of rocks by diffusive mass transfer (pressure solution) in nature which are pertinent to the rate controlling mechanism of the deformation are reviewed, and it is inferred that (a) the diffusion of matter in an aqueous intergranular film which can support shear stress is an essential part of the process, and (b) the diffusion is driven by stress induced chemical potential gradients, together with gradients due to local chemical reactions.</jats:p>\n          <jats:p>The theoretical approach to the derivation of constitutive flow laws for creep by diffusive mass transfer is outlined, and a simplified flow law proposed. Crucial to the absolute rate of deformation predicted by the flow law is the estimation of the phenomenological coefficient which links diffusive flux to chemical potential gradient. It is argued that this should be several orders of magnitude less in thin, stressed aqueous films than for solutions of ions in large water volumes.</jats:p>\n          <jats:p>Some simple experiments are described to address the question of (a) the existence of thin intergranular aqueous films which can support shear stress, and(b) the magnitude of the above phenomenological coefficient. The results obtained are consistent with the inferences made from the study of microstructures in naturally deformed rocks, and this is illustrated by means of extrapolation of theoreticallv derived relationships to conditions of natural rock deformation and sediment compaction by pressure solution.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1580572701439466752","@type":"Researcher","foaf:name":[{"@value":"E. H. Rutter"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167649"},{"@type":"EISSN","@value":"2041479X"},{"@type":"NCID","@value":"AA00698835"}],"prism:publicationName":[{"@value":"Journal of the Geological Society"}],"dc:publisher":[{"@value":"Geological Society of London"}],"prism:publicationDate":"1983-09","prism:volume":"140","prism:number":"5","prism:startingPage":"725","prism:endingPage":"740"},"reviewed":"false","dc:rights":["https://doi.org/10.15223/policy-002"],"url":[{"@id":"https://www.lyellcollection.org/doi/pdf/10.1144/gsjgs.140.5.0725"}],"createdAt":"2007-12-20","modifiedAt":"2024-11-19","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360285708267186304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Propagation dynamics of seismic and aseismic slip governed by fault heterogeneity and Newtonian rheology"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302866835045632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rapid Fault Healing After Seismic Slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306904387728384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Frictional Properties and Healing Behavior of Tectonic Mélanges: Implications for the Evolution of Subduction Fault Zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182379024384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Silicate diffusion in alkali-carbonatite and hydrous melts at 16.5 and 24 GPa: Implication for the melt transport by dissolution–precipitation in the transition zone and uppermost lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580229782278272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Embrittlement Within Viscous Shear Zones Across the Base of the Subduction Thrust Seismogenic Zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657255058304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Grain-size-sensitive creep of plagioclase accompanied by solution–precipitation and mass transfer under mid-crustal conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512078848","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Frictional behavior of synthetic gouge-bearing faults under the operation of pressure solution"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680741712128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Long-term Observation of Permeability in Sedimentary Rocks under High Temperature and Stress Conditions and Its Interpretation Mediated by Microstructural Investigations"},{"@value":"Long‐term observation of permeability in sedimentary rocks under high‐temperature and stress conditions and its interpretation mediated by microstructural investigations"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488789376","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fluid pressure evolution during the earthquake cycle controlled by fluid flow and pressure solution crack sealing"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417117554432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Elastic wave velocity and electrical conductivity in a brine-saturated rock and microstructure of pores"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317073909760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Simultaneous measurements of elastic wave velocities and electrical conductivity in a brine-saturated granitic rock under confining pressures and their implication for interpretation of geophysical observations"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1144/gsjgs.140.5.0725"},{"@type":"CIA","@value":"30031598338"},{"@type":"CROSSREF","@value":"10.1186/bf03353315_references_DOI_Tpx6qct9W7dNND4l6D3nPTV7Esx"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2013.09.004_references_DOI_Tpx6qct9W7dNND4l6D3nPTV7Esx"},{"@type":"CROSSREF","@value":"10.1016/j.jsg.2013.03.006_references_DOI_Tpx6qct9W7dNND4l6D3nPTV7Esx"},{"@type":"CROSSREF","@value":"10.1029/2012jb009532_references_DOI_Tpx6qct9W7dNND4l6D3nPTV7Esx"},{"@type":"CROSSREF","@value":"10.1029/2023jb026706_references_DOI_Tpx6qct9W7dNND4l6D3nPTV7Esx"},{"@type":"CROSSREF","@value":"10.1029/2023jb028472_references_DOI_Tpx6qct9W7dNND4l6D3nPTV7Esx"},{"@type":"CROSSREF","@value":"10.1186/s40645-015-0067-0_references_DOI_Tpx6qct9W7dNND4l6D3nPTV7Esx"},{"@type":"CROSSREF","@value":"10.1002/2014wr016427_references_DOI_Tpx6qct9W7dNND4l6D3nPTV7Esx"},{"@type":"CROSSREF","@value":"10.1029/2021gc010208_references_DOI_Tpx6qct9W7dNND4l6D3nPTV7Esx"},{"@type":"CROSSREF","@value":"10.1186/bf03353316_references_DOI_Tpx6qct9W7dNND4l6D3nPTV7Esx"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1112-9_references_DOI_Tpx6qct9W7dNND4l6D3nPTV7Esx"}]}