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Leader		00000nz a2200037n 45 0
001		WKP\|Q67217991 (VIAF cluster) (Authority/Source Record)
003		WKP
005		20241120235806.0
008		241120nneanz\|\|abbn n and d
035		‎‡a (WKP)Q67217991‏
024		‎‡a 0000-0002-6925-5373‏ ‎‡2 orcid‏
024		‎‡a 7406327128‏ ‎‡2 scopus‏
035		‎‡a (OCoLC)Q67217991‏
100	0	‎‡a Scott Johnson‏ ‎‡9 ast‏
400	0	‎‡a স্কট জনসন‏ ‎‡9 bn‏
400	0	‎‡a Scott E. Johnson‏ ‎‡c researcher (ORCID 0000-0002-6925-5373)‏ ‎‡9 en‏
400	0	‎‡a Scott Johnson‏ ‎‡c investigador‏ ‎‡9 es‏
400	0	‎‡a Scott Johnson‏ ‎‡c wetenschapper‏ ‎‡9 nl‏
670		‎‡a Author's Computational homogenization and micromechanical analysis of textured polycrystalline materials‏
670		‎‡a Author's Coseismic damage runs deep in continental strike-slip faults‏
670		‎‡a Author's Crack extension induced by dissociation of fracture-hosted methane gas hydrate‏
670		‎‡a Author's Elastic Contrast, Rupture Directivity, and Damage Asymmetry in an Anisotropic Bimaterial Strike-Slip Fault at Middle Crustal Depths‏
670		‎‡a Author's Energy Partitioning, Dynamic Fragmentation, and Off‐Fault Damage in the Earthquake Source Volume‏
670		‎‡a Author's Growth rates of dike-fed plutons: Are they compatible with observations in the middle and upper crust?‏
670		‎‡a Author's Identifying deformed pseudotachylyte and its influence on the strength and evolution of a crustal shear zone at the base of the seismogenic zone‏
670		‎‡a Author's Implications of rapid, dike-fed pluton growth for host-rock strain rates and emplacement mechanisms‏
670		‎‡a Author's Mica kink-band geometry as an indicator of coseismic dynamic loading‏
670		‎‡a Author's Modification of crustal seismic anisotropy by geological structures‏
670		‎‡a Author's Modification of crustal seismic anisotropy by geological structures ( “structural geometric anisotropy” )‏
670		‎‡a Author's Pervasive cracking of heterogeneous brittle materials using a multi-directional smeared crack band model‏
670		‎‡a Author's Porphyroblast rotation and strain localization: Debate settled!: REPLY‏
670		‎‡a Author's Quartz fluid inclusion abundance and off-fault damage in a deeply exhumed, strike-slip, seismogenic fault‏
670		‎‡a Author's Recrystallization fabrics of sheared quartz veins with a strong pre-existing crystallographic preferred orientation from a seismogenic shear zone‏
670		‎‡a Author's Subvolcanic and Deep-Crustal Tonalite Genesis beneath the Mexican Peninsular Ranges‏
670		‎‡a Author's The effect of microstructural and rheological heterogeneity on porphyroblast kinematics and bulk strength in porphyroblastic schists‏
670		‎‡a Author's The influence of crenulation cleavage development on the bulk elastic and seismic properties of phyllosilicate-rich rocks‏
670		‎‡a Author's The influence of microstructure on seismic wave speed anisotropy in the crust: computational analysis of quartz-muscovite rocks‏
670		‎‡a Author's The quartz α↔β phase transition: Does it drive damage and reaction in continental crust?‏
670		‎‡a Author's Using zircon U–Pb ages and trace element chemistry to constrain the timing of metamorphic events, pegmatite dike emplacement, and shearing in the southern Parry Sound domain, Grenville Province, Canada‏
909		‎‡a (orcid) 0000000269255373‏ ‎‡9 1‏
909		‎‡a (scopus) 7406327128‏ ‎‡9 1‏
919		‎‡a influenceofmicrostructureonseismicwavespeedanisotropyinthecrustcomputationalanalysisofquartzmuscoviterocks‏ ‎‡A The influence of microstructure on seismic wave speed anisotropy in the crust: computational analysis of quartz-muscovite rocks‏ ‎‡9 1‏
919		‎‡a micakinkbandgeometryasanindicatorofcoseismicdynamicloading‏ ‎‡A Mica kink-band geometry as an indicator of coseismic dynamic loading‏ ‎‡9 1‏
919		‎‡a energypartitioningdynamicfragmentationandofffaultdamageintheearthquakesourcevolume‏ ‎‡A Energy Partitioning, Dynamic Fragmentation, and Off‐Fault Damage in the Earthquake Source Volume‏ ‎‡9 1‏
919		‎‡a coseismicdamagerunsdeepincontinentalstrikeslipfaults‏ ‎‡A Coseismic damage runs deep in continental strike-slip faults‏ ‎‡9 1‏
919		‎‡a computationalhomogenizationandmicromechanicalanalysisoftexturedpolycrystallinematerials‏ ‎‡A Computational homogenization and micromechanical analysis of textured polycrystalline materials‏ ‎‡9 1‏
919		‎‡a elasticcontrastrupturedirectivityanddamageasymmetryinananisotropicbimaterialstrikeslipfaultatmiddlecrustaldepths‏ ‎‡A Elastic Contrast, Rupture Directivity, and Damage Asymmetry in an Anisotropic Bimaterial Strike-Slip Fault at Middle Crustal Depths‏ ‎‡9 1‏
919		‎‡a crackextensioninducedbydissociationoffracturehostedmethanegashydrate‏ ‎‡A Crack extension induced by dissociation of fracture-hosted methane gas hydrate‏ ‎‡9 1‏
919		‎‡a growthratesofdikefedplutonsaretheycompatiblewithobservationsinthemiddleanduppercrust‏ ‎‡A Growth rates of dike-fed plutons: Are they compatible with observations in the middle and upper crust?‏ ‎‡9 1‏
919		‎‡a implicationsofrapiddikefedplutongrowthforhostrockstrainratesandemplacementmechanisms‏ ‎‡A Implications of rapid, dike-fed pluton growth for host-rock strain rates and emplacement mechanisms‏ ‎‡9 1‏
919		‎‡a modificationofcrustalseismicanisotropybygeologicalstructures‏ ‎‡A Modification of crustal seismic anisotropy by geological structures‏ ‎‡9 1‏
919		‎‡a pervasivecrackingofheterogeneousbrittlematerialsusingamultidirectionalsmearedcrackbandmodel‏ ‎‡A Pervasive cracking of heterogeneous brittle materials using a multi-directional smeared crack band model‏ ‎‡9 1‏
919		‎‡a identifyingdeformedpseudotachylyteanditsinfluenceonthestrengthandevolutionofacrustalshearzoneatthebaseoftheseismogeniczone‏ ‎‡A Identifying deformed pseudotachylyte and its influence on the strength and evolution of a crustal shear zone at the base of the seismogenic zone‏ ‎‡9 1‏
919		‎‡a quartzfluidinclusionabundanceandofffaultdamageinadeeplyexhumedstrikeslipseismogenicfault‏ ‎‡A Quartz fluid inclusion abundance and off-fault damage in a deeply exhumed, strike-slip, seismogenic fault‏ ‎‡9 1‏
919		‎‡a recrystallizationfabricsofshearedquartzveinswithastrongpreexistingcrystallographicpreferredorientationfromaseismogenicshearzone‏ ‎‡A Recrystallization fabrics of sheared quartz veins with a strong pre-existing crystallographic preferred orientation from a seismogenic shear zone‏ ‎‡9 1‏
919		‎‡a porphyroblastrotationandstrainlocalizationdebatesettledreply‏ ‎‡A Porphyroblast rotation and strain localization: Debate settled!: REPLY‏ ‎‡9 1‏
919		‎‡a effectofmicrostructuralandrheologicalheterogeneityonporphyroblastkinematicsandbulkstrengthinporphyroblasticschists‏ ‎‡A The effect of microstructural and rheological heterogeneity on porphyroblast kinematics and bulk strength in porphyroblastic schists‏ ‎‡9 1‏
919		‎‡a modificationofcrustalseismicanisotropybygeologicalstructuresstructuralgeometricanisotropy‏ ‎‡A Modification of crustal seismic anisotropy by geological structures ( “structural geometric anisotropy” )‏ ‎‡9 1‏
919		‎‡a quartzαβphasetransitiondoesitdrivedamageandreactionincontinentalcrust‏ ‎‡A The quartz α↔β phase transition: Does it drive damage and reaction in continental crust?‏ ‎‡9 1‏
919		‎‡a influenceofcrenulationcleavagedevelopmentonthebulkelasticandseismicpropertiesofphyllosilicaterichrocks‏ ‎‡A The influence of crenulation cleavage development on the bulk elastic and seismic properties of phyllosilicate-rich rocks‏ ‎‡9 1‏
919		‎‡a usingzirconupbagesandtraceelementchemistrytoconstrainthetimingofmetamorphiceventspegmatitedikeemplacementandshearinginthesouthernparrysounddomaingrenvilleprovincecanada‏ ‎‡A Using zircon U–Pb ages and trace element chemistry to constrain the timing of metamorphic events, pegmatite dike emplacement, and shearing in the southern Parry Sound domain, Grenville Province, Canada‏ ‎‡9 1‏
919		‎‡a subvolcanicanddeepcrustaltonalitegenesisbeneaththemexicanpeninsularranges‏ ‎‡A Subvolcanic and Deep-Crustal Tonalite Genesis beneath the Mexican Peninsular Ranges‏ ‎‡9 1‏
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