{"@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/1360580229804889600.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.5194/egusphere-2022-1487"}},{"identifier":{"@type":"DOI","@value":"10.5194/se-14-409-2023"}},{"identifier":{"@type":"URI","@value":"https://se.copernicus.org/articles/14/409/2023/se-14-409-2023.pdf"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Water release and homogenization by dynamic recrystallization of quartz"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Abstract. To evaluate changes in water distribution generated by dynamic recrystallization of quartz, we performed infrared (IR) spectroscopy mapping of quartz in deformed granite from the Wariyama uplift zone in NE Japan. We analyzed three granite samples with different degrees of deformation: almost undeformed, weakly deformed, and strongly deformed. Dynamically recrystallized quartz grains with a grain size of ~10 µm are found in these three samples, but the percentages of recrystallized grains and recrystallization processes are different. Quartz in the almost undeformed sample shows wavy grain boundaries with a few bulged quartz grains. In the weakly deformed sample, bulging of quartz is developed in regions a few hundred micrometers from adjacent host quartz grains. In the strongly deformed sample, almost all quartz grains are recrystallized by subgrain rotation. IR spectra of quartz in the three samples commonly show a broad water band owing to H2O fluid at 2800–3750 cm−1 with no structural OH bands. Water contents in host quartz grains in the almost undeformed sample are in the range of 40–1750 wt. ppm, with a mean of 500 ± 280 wt. ppm H2O. On the other hand, water contents in regions of recrystallized grains, regardless of the recrystallization processes involved, are in the range of 100–510 wt. ppm, with a mean of 220 ± 70 wt. ppm, which are low and homogeneous compared with contents in host quartz grains. Water contents in regions of subgrains are intermediate between those in host and recrystallized grains. These results for water distribution in quartz imply that water is released by dynamic recrystallization.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420001326228742144","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"10726764"},{"@type":"NRID","@value":"1000010726764"},{"@type":"NRID","@value":"9000002103223"},{"@type":"NRID","@value":"9000014284948"},{"@type":"NRID","@value":"9000350559701"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/junichifukuda"}],"foaf:name":[{"@value":"Junichi Fukuda"}]},{"@id":"https://cir.nii.ac.jp/crid/1380580229804889601","@type":"Researcher","foaf:name":[{"@value":"Takamoto Okudaira"}]},{"@id":"https://cir.nii.ac.jp/crid/1380580229804889602","@type":"Researcher","foaf:name":[{"@value":"Yukiko Ohtomo"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18699529"}],"prism:publicationName":[{"@value":"Solid Earth"}],"dc:publisher":[{"@value":"Copernicus GmbH"}],"prism:publicationDate":"2023-01-02","prism:volume":"14","prism:number":"4","prism:startingPage":"409","prism:endingPage":"424"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://creativecommons.org/licenses/by/4.0/"],"url":[{"@id":"https://se.copernicus.org/articles/14/409/2023/se-14-409-2023.pdf"}],"createdAt":"2023-01-02","modifiedAt":"2023-04-19","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=QE1-996.5","dc:title":"QE1-996.5"},{"@id":"https://cir.nii.ac.jp/all?q=Stratigraphy","dc:title":"Stratigraphy"},{"@id":"https://cir.nii.ac.jp/all?q=Geology","dc:title":"Geology"},{"@id":"https://cir.nii.ac.jp/all?q=QE640-699","dc:title":"QE640-699"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040282256994048896","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"19K04041"},{"@type":"JGN","@value":"JP19K04041"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-19K04041/"}],"notation":[{"@language":"ja","@value":"天然変形岩から評価する地殻の塑性変形強度"},{"@language":"en","@value":"Plastic strength of the crust evaluated from naturally deformed rocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1040295802071680384","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23K03531"},{"@type":"JGN","@value":"JP23K03531"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23K03531/"}],"notation":[{"@language":"ja","@value":"上部地殻のレオロジーを支配する石英の優先すべり系の確定"},{"@language":"en","@value":"Determination of the dominant slip system in quartz and its importance to the upper crustal rheology"}]},{"@id":"https://cir.nii.ac.jp/crid/1040848250652948352","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"20K04087"},{"@type":"JGN","@value":"JP20K04087"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-20K04087/"}],"notation":[{"@language":"ja","@value":"大阪平野における活断層の3次元構造：地表付近から地震発生領域まで"},{"@language":"en","@value":"Three dimensional structure of active faults in Osaka Plain from surface to seismogenic zone"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050012570392438528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Water distribution in quartz schists of the Sanbagawa Metamorphic Belt, Japan: infrared spectroscopic mapping and comparison of the calibrations proposed for determining water contents"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142941004544","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rheology of the upper mantle and the mantle wedge: A view from the experimentalists"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144031806592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Characterization of the states and diffusivity of intergranular water in a chalcedonic quartz by high-temperature <i>in situ</i> infrared spectroscopy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144838220288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Dry and strong quartz during deformation of the lower crust in the presence of melt"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013172384865920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Solubility and diffusional uptake of hydrogen in quartz at high water pressures: Implications for hydrolytic weakening"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021394455894912","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modification of fluid inclusions in quartz by deviatoric stress I: experimentally induced changes in inclusion shapes and microstructures"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021394456280448","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effect of pressure on the deformation of quartz aggregates in the presence of H2O"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021394457010432","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Influence of dislocations on water leakage from fluid inclusions in quartz: a quantitative reappraisal"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285705096448000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Water content of the mantle xenoliths from Kimberley and implications for explaining textural variations in cratonic roots"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707500031104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Solution–precipitation of K-feldspar in deformed granitoids and its relationship to the distribution of water"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292618959367040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Water-Induced Fabric Transitions in Olivine"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292618963836416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Dissociated ?a? dislocations in quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619206503808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effects of chemical environment on dislocation creep of quartzite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620207809152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Synchrotron FTIR imaging of OH in quartz mylonites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621415926400","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deformation of Fine‐Grained Quartz Aggregates by Mixed Diffusion and Dislocation Creep"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294645631234560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Plastic-deformati on mechanisms in quartz: The effect of water"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294646913752192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Some effects of tectonic recrystallisation on fluid inclusions in vein quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094411905152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The recrystallized grain size piezometer for quartz: An EBSD‐based calibration"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094773016320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The eastern Tonale fault zone: a ‘natural laboratory’ for crystal plastic deformation of quartz over a temperature range from 250 to 700°C"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095058925568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deformation of Granitic Rocks: Experimental Studies and Natural Examples"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095899785856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effect of aqueous and carbonic fluids on the dislocation creep strength of quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096245257600","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The determination of hydroxyl by infrared absorption in quartz, silicate glasses and similar materials"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096280464256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Dislocation creep of dry quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096388287360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Water distribution in low-grade siliceous metamorphic rocks by micro-FTIR and its relation to grain size: a case from the Kanto Mountain region, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096436055040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Shear zones – A review"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584343733069696","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The influence of water and LPO on the initiation and evolution of mantle shear zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584343733545216","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quartz Flow Law Revisited: The Significance of Pressure Dependence of the Activation Enthalpy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345418988032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Natural and Experimental Constraints on a Flow Law for Dislocation‐Dominated Creep in Wet Quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345418993920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reaction of Hydrogen Peroxide and Nitric Oxide"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345419812096","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"OH point defects in quartz – a review"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584346086053632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Fluid inclusions, deformation and recrystallization in granite tectonites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584346086341760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Enrichment of CO2 in fluid inclusions in quartz by removal of H2O during crystal-plastic deformation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584346087411456","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Water loss during dynamic recrystallization of Moine thrust quartzites, northwest Scotland"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584346087507840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The infrared absorption band at 3596 cm<sup>−1</sup> of the recrystallized\n                  quartz from Mt. Takamiyama, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654736679680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Theoretical derivation of flow laws for quartz dislocation creep: Comparisons with experimental creep data and extrapolation to natural conditions using water fugacity corrections"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855568465775360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effect of water and stress on the lattice-preferred orientation of olivine"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569135439872","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evolution in H2O contents during deformation of polycrystalline quartz: An experimental study"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569369600000","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hydrolytic weakening and penetrative deformation within a natural shear zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569640815488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Microinfrared reflection spectroscopic mapping: application to the detection of hydrogen‐related species in natural quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570303542784","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An IR absorption calibration for water in minerals"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570810274304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The role of tectonic grain size reduction in the rheological stratification of the lithosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570878253952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Strength of the lithosphere: Constraints imposed by laboratory experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571127719168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"New type of olivine fabric from deformation experiments at modest water content and low stress"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571286824576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rheology of the Lower Crust and Upper Mantle: Evidence from Rock Mechanics, Geodesy, and Field Observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043618918528","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rapid contamination during storage of carbonaceous chondrites prepared for micro FTIR measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043720124928","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A natural example of crystal-plastic deformation enhancing the incorporation of water into quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043848450432","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Crystal preferred orientations of olivine, orthopyroxene, serpentine, chlorite, and amphibole, and implications for seismic anisotropy in subduction zones: a review"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044409396224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Theory and Applicability of a Recrystallized Grain Size Paleopiezometer"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519453486208","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Fluids in the lithosphere, 1. Experimentally-determined wetting characteristics of CO2H2O fluids and their implications for fluid transport, host-rock physical properties, and fluid inclusion formation"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520795556352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Water distribution in dynamically recrystallized quartz grains: cathodoluminescence and micro-infrared spectroscopic mapping"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995799771008","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Infrared microspectroscopy analysis of water distribution in deformed and metamorphosed rocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995823320064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Fourier transform infrared spectroscopy determinations of intragranular water content in quartz-bearing rocks: implications for hydrolytic weakening in the laboratory and within the earth"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995833180032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The effect of varying water contents on the creep behavior of Heavitree quartzite"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470003875584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Anisotropic high-temperature creep in hydrous olivine single crystals and its geodynamic implications"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943953278208","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Accurate differential stress measurement using the molten salt cell and solid salt assemblies in the Griggs apparatus with applications to strength, piezometers and rheology"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944452142592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geodynamic Significance of Seismic Anisotropy of the Upper Mantle: New Insights from Laboratory Studies"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945053625600","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Water loss and the origin of thick ultramylonites"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945214095872","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quartz recrystallization regimes, c-axis texture transitions and fluid inclusion reequilibration in a prograde greenschist to amphibolite facies mylonite zone (Ribeira Shear Zone, SE Brazil)"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945485087744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Water redistribution in experimentally deformed natural milky quartz single crystals—Implications for H<sub>2</sub>O‐weakening processes"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945660007680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Equilibrium dihedral angles in the system quartz-CO2H2ONaCl at 800°C and 1–15 kbar: the effects of pressure and fluid composition on the permeability of quartzites"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419257124352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Water precipitation and diffusion in wet quartz and wet berlinite AIPO4"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420238387584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hydrolytic Weakening of Quartz and Other Silicates*"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420309553408","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Theories and applicability of grain size piezometers: The role of dynamic recrystallization mechanisms"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544421160808064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quartz: Anomalous Weakness of Synthetic Crystals"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893381961088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effect of water on the dislocation creep microstructure and flow stress of quartz and implications for the recrystallized grain size piezometer"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894432978432","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The recrystallized grain size piezometer for quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369218952064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Steady-State Grain Size in Dynamic Recrystallization of Minerals"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369716727040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Temperature and pressure dependence of quartz-aqueous fluid dihedral angles: the control of adsorbed H2O on the permeability of quartzites"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369907651584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A survey of hydrous species and concentrations in igneous feldspars"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369913785088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hydrogen speciation in synthetic quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843497242112","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The role of fluids in low temperature, fault-related deformation of quartz arenite"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844759601280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Chapter 4. HYDROGEN SPECIATION AND CHEMICAL WEAKENING OF QUARTZ"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845861449472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Water in minerals? A peak in the infrared"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318443841536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The structure of grain boundaries in granite-origin ultramylonite studied by high-resolution electron microscopy"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320064902400","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Flow laws and fabric transitions in wet quartzite"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320695675008","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reversible water weakening of quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793368267776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Finite-element folds of similar geometry"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793440786816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Synthetic fluid inclusions. XV. TEM investigation of plastic flow associated with reequilibration of fluid inclusions in natural quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794155603200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Oblique subduction, collision of microcontinents and subduction of oceanic ridge: Their implications on the Cretaceous tectonics of Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795458705536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Flow strengths of quartz aggregates: Grain size and pressure effects due to hydrolytic weakening"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268835352064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effect of water on the rheology of experimentally deformed quartzite"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270910882560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"IR calibrations for water determination in olivine, r-GeO2, and SiO2 polymorphs"}]},{"@id":"https://cir.nii.ac.jp/crid/1390025960460586112","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fluid behavior in rocks during grain growth: insights from analogue experiments using camphor-ethanol mixtures"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681216693248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Zircon U–Pb age and its geological significance of late Carboniferous and Early Cretaceous adakitic granites from eastern margin of the Abukuma Mountains, Japan"},{"@language":"ja","@value":"阿武隈山地東縁の石炭紀および白亜紀アダカイト質花崗岩類とその地質学的意義"},{"@value":"Zircon U-Pb age and its geological significance of the late Carboniferous and Early Cretaceous adakitic granites from eastern margin of the Abukuma Mountains, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217856256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Late Carboniferous and Early Cretaceous adakitic granites from eastern margin of the Abukuma Mountains"},{"@language":"ja","@value":"阿武隈山地東縁の石炭紀および白亜紀アダカイト質花崗岩類"}]},{"@id":"https://cir.nii.ac.jp/crid/1390301330606010752","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Exploring the Eastern Abukuma Mountains: A field guide to high-pressure metamorphic rocks and strike-slip crustal shear zones in the Southern Kitakami Belt, NE Japan"},{"@language":"ja","@value":"阿武隈山地東縁を探る：南部北上帯の高圧型片岩類と横ずれ剪断帯のフィールドガイド"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.5194/egusphere-2022-1487"},{"@type":"CROSSREF","@value":"10.5194/se-14-409-2023"},{"@type":"KAKEN","@value":"PRODUCT-24519534"},{"@type":"KAKEN","@value":"PRODUCT-24952910"},{"@type":"KAKEN","@value":"PRODUCT-24998455"},{"@type":"OPENAIRE","@value":"doi_dedup___::990226bb5f8236c22bcd1001ba61a02d"},{"@type":"CROSSREF","@value":"10.5194/se-14-409-2023_references_DOI_KTY4v6UMUMeycLAVjRRD2Tp17pF"},{"@type":"CROSSREF","@value":"10.2465/jmps.250603_references_DOI_3zoE65BhBHP3O8NGkyAkA5G0W4u"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2024.0022_references_DOI_3zoE65BhBHP3O8NGkyAkA5G0W4u"},{"@type":"CROSSREF","@value":"10.5194/egusphere-2022-1487_isPreprintOf_DOI_3zoE65BhBHP3O8NGkyAkA5G0W4u"},{"@type":"CROSSREF","@value":"10.5194/se-14-409-2023_hasPreprint_DOI_KTY4v6UMUMeycLAVjRRD2Tp17pF"}]}