Grainsize evolution in ductile shear zones: Implications for strain localization and the strength of the lithosphere

No abstract is available for this paper.

• Publication year

  2011

• Venue

  Journal of Structural Geology

• Publication date

  2011-04-01

• Fields of study

  Geology

• Identifiers
  DOI 10.1016/J.JSG.2011.01.018
• External record

  Open on Semantic Scholar

• Source metadata

  Semantic Scholar

• No claims are published for this paper.

• No concepts are published for this paper.

• Diffusion Data for Silicate Minerals, Glasses, and Liquids

  2013cited by this paper
• Rheology of the Upper Mantle and the Mantle Wedge: A View from the Experimentalists

  2013influential reference
• Lithospheric shear zones as constant stress experiments

  2011cited by this paper
• A naturally constrained stress profile through the middle crust in an extensional terrane

  2011cited by this paper
• A new perspective on paleopiezometry: Dynamically recrystallized grain size distributions indicate mechanism changes

  2010cited by this paper
• Accurate differential stress measurement using the molten salt cell and solid salt assemblies in the Griggs apparatus with applications to strength, piezometers and rheology

  2010cited by this paper
• Dislocation Mean Free Paths and Strain Hardening of Crystals

  2008influential reference
• Theories and applicability of grain size piezometers : The role of dynamic recrystallization mechanisms

  2008influential reference
• Dynamic recrystallization near the brittle-plastic transition in naturally and experimentally deformed quartz aggregates

  2008cited by this paper
• Strain localisation in the subcontinental mantle — a ductile alternative to the brittle mantle

  2007cited by this paper
• Continental Fault Structure and Rheology from the Frictional-to-Viscous Transition Downward

  2007influential reference
• Tectonic Faults: Agents of Change on a Dynamic Earth

  2007cited by this paper
• Paleowattmeters: A scaling relation for dynamically recrystallized grain size

  2007influential reference
• The effect of energy feedbacks on continental strength

  2006cited by this paper
• Dynamic recrystallization and strain softening of olivine aggregates in the laboratory and the lithosphere

  2005cited by this paper
• Experimental intracrystalline plastic flow in hot-pressed synthetic quartzite prepared from Brazilian quartz crystals

  2004cited by this paper
• Experimental grain size-sensitive flow of hot-pressed Brazilian quartz aggregates

  2004cited by this paper
• Recrystallization and Grain Growth

  2004influential reference
• Grain size evolution and the rheology of ductile shear zones: from laboratory experiments to postseismic creep

  2003cited by this paper
• Influence of grain size evolution on convective instability

  2003cited by this paper
• The recrystallized grain size piezometer for quartz

  2003influential reference
• Inside the subduction factory

  2003cited by this paper
• The generation of plate tectonics from mantle convection

  2003cited by this paper
• Microstructural Evidence for Grain Size Sensitive Deformation Mechanisms in Naturally Deformed Peridotites

  2002cited by this paper
• A unified description of localization for application to large-scale tectonics

  2002cited by this paper
• Interfacial energies for quartz and albite in pelitic schist

  2002influential reference
• Dynamic recrystallization of quartz: correlation between natural and experimental conditions

  2002influential reference
• The eastern Tonale fault zone: a ‘natural laboratory’ for crystal plastic deformation of quartz over a temperature range from 250 to 700 °C

  2002influential reference
• Si and O diffusion in olivine and implications for characterizing plastic flow in the mantle

  2002cited by this paper
• Grain boundary energies in olivine derived from natural microstructures

  2001influential reference
• An evaluation of quartzite flow laws based on comparisons between experimentally and naturally deformed rocks

  2001cited by this paper
• A few remarks on the kinetics of static grain growth in rocks

  2001cited by this paper
• Grain size reduction by dynamic recrystallization: can it result in major rheological weakening?

  2001influential reference
• Silicon diffusion in forsterite aggregates: Implications for diffusion accommodated creep

  2000cited by this paper
• Mantle convection and plate tectonics: toward an integrated physical and chemical theory

  2000cited by this paper
• Silicon diffusion in a natural quartz aggregate: constraints on solution-transfer diffusion creep

  2000cited by this paper
• A simple parameterization of strain localization in the ductile regime due to grain size reduction: A case study for olivine

  1999cited by this paper
• An internally consistent thermodynamic data set for phases of petrological interest

  1998cited by this paper
• Stress and temperature dependence of recrystallized grain size: A subgrain misorientation model

  1998influential reference
• Mechanisms of shear localization in the continental lithosphere: inference from the deformation microstructures of peridotites from the Ivrea zone, northwestern Italy

  1998cited by this paper
• On dynamic recrystallization during solid state flow: Effects of stress and temperature

  1998influential reference
• Mantle convection simulations with rheologies that generate plate-like behaviour

  1998cited by this paper
• Thermomechanical evolution of a ductile duplex

  1997cited by this paper
• ABYSSAL PERIDOTITE MYLONITES : IMPLICATIONS FOR GRAIN-SIZE SENSITIVE FLOW AND STRAIN LOCALIZATION IN THE OCEANIC LITHOSPHERE

  1996cited by this paper
• DEFORMATION-ENHANCED FLUID DISTRIBUTION IN FELDSPAR AGGREGATES AND IMPLICATIONS FOR DUCTILE SHEAR ZONES

  1996cited by this paper
• Interaction of weak faults and non-newtonian rheology produces plate tectonics in a 3D model of mantle flow

  1996cited by this paper
• Recrystallization and Related Annealing Phenomena

  1995influential reference
• Quartz deformation in a very fine grained quartzo-feldspathic mylonite: a lack of evidence for dominant grain boundary sliding deformation

  1995cited by this paper
• Experimental study of the influence of stress, temperature, and strain on the dynamic recrystallization of Carrara marble

  1995cited by this paper
• EQUATIONS OF STATE VALID CONTINUOUSLY FROM ZERO TO EXTREME PRESSURES FOR H2O AND CO2

  1994influential reference
• Relationships between dynamically recrystallized grain size and deformation conditions in experimentally deformed olivine rocks

  1993influential reference
• Rheology of the Upper Mantle: A Synthesis

  1993cited by this paper
• The rheology of faults triggered by the olivine-spinel transformation in Mg2GeO4 and its implications for the mechanism of deep-focus earthquakes

  1993cited by this paper
• Dislocation creep regimes in quartz aggregates

  1992influential reference
• Dynamic recrystallisation: The steady state grain size

  1992cited by this paper
• Rheology of solids and of the earth

  1992cited by this paper
• The dependence of grain size on stress during dynamic recrystallisation

  1991influential reference
• Experimental study of grain-size sensitive flow of synthetic, hot-pressed calcite rocks

  1990cited by this paper
• Grain growth kinetics in olivine aggregates

  1989cited by this paper
• Internally consistent thermodynamic data for minerals in the system Na2O-K2O-CaO-MgO-FeO-F

  1988cited by this paper
• The role of tectonic grain size reduction in the rheological stratification of the lithosphere

  1988cited by this paper
• On Dynamic Recrystallization

  1987influential reference
• The role of transiently fine-grained reaction products in syntectonic metamorphism: natural and experimental examples

  1987cited by this paper
• Grain-boundary migration microstructures in a naturally deformed quartzite

  1987cited by this paper
• On dynamic recrystallisation

  1987influential reference
• Dynamic recrystallization of feldspar: A mechanism for ductile shear zone formation

  1985cited by this paper
• Surface and interfacial free energies of quartz

  1984influential reference
• Grain Growth Kinetics of Quartz and Calcite Aggregates

  1982cited by this paper
• High temperature flow and dynamic recrystallization in carrara marble

  1980influential reference
• Stress dependence of recrystallized-grain and subgrain size in olivine

  1980influential reference
• Deformation‐induced microstructures, paleopiezometers, and differential stresses in deeply eroded fault zones

  1980influential reference
• Shear localization and shear instability in materials in the ductile field

  1980influential reference
• Grainsize reduction, grain boundary sliding and the flow strength of mylonites

  1979cited by this paper
• Transformation- and reaction-enhanced ductility in rocks

  1978cited by this paper
• Theory and applicability of a recrystallized grain size paleopiezometer

  1977influential reference
• A Discussion on natural strain and geological structure - The effects of strain on the microstructures, fabrics, and deformation mechanisms in quartzites

  1976cited by this paper
• On the Creep of Crystals

  1971cited by this paper

• Multiple-stage evolution of the Cenozoic ductile deformation in the Tethyan orogenic belt constrained via single-grain mica Rb Sr isochron ages

  2026cites this paper
• Strain energy-driven grain growth in quartz aggregates: Implications for microstructural evolution and recovery

  2026cites this paper
• Mineralogical and deformational signatures of the Neogene Surma Group sandstones in the Bengal Basin from high-resolution petrography and provenance

  2026cites this paper
• The Rheological Evolution of Granitic Rocks in the Middle and Lower Crust

  2026cites this paper
• Controls on Asymmetric Continental Crustal Thinning to Symmetric Mantle Exhumation at Magma‐Poor Rifted Margins: Processes Constrained by the West Iberia‐Newfoundland Conjugate Margins

  2025cites this paper
• Grain-size reduction diminishes the impact of viscous shear heating in lithospheric mantle shear zones

  2025cites this paper
• In-situ tensile deformation of high Sulfur Gadolinium bearing steels

  2025cites this paper
• The temporal and kinematic constraints on the early Alpine orogen: insights from Rb–Sr geochronology and geological mapping of the Avers nappe (Eastern Swiss-Alps)

  2025cites this paper
• Evolution of Nanocavities to Ductile Fractures in Crustal‐Scale Faults at the Base of the Seismogenic Zone

  2025cites this paper
• Dissolution–precipitation creep in polymineralic granitoid shear zones in experiments – Part 1: Strain localization mechanisms

  2025cites this paper
• Strain Localization and Seismic Properties in the Heterogeneous Ailaoshan‐Red River Shear Zone, Southeast Asia

  2025cites this paper
• Hydration of mafic crustal rocks at high temperature during brittle‐viscous deformation along a strike‐slip plate boundary

  2024cites this paper
• Elastic thermobarometry on metapelites across the crustal section of the Famatinian Arc, Argentina

  2024cites this paper
• Transient and Steady‐State Friction in Non‐Isobaric Conditions

  2024cites this paper
• The Samail subduction zone dilemma: Geochronology of high-pressure rocks from the Saih Hatat window, Oman, reveals juxtaposition of two subduction zones with contrasting thermal histories

  2024cites this paper
• Localization and Delocalization During Seismic Slip

  2024cites this paper
• Strain rates recorded in the perimeter-area relationship of recrystallized quartz aggregates from the Sandhill Corner shear zone, Maine, USA

  2024cites this paper
• Interrogating an along-strike variation in the evolution and rheology of a large continental strike-slip fault zone

  2024cites this paper
• Dynamic Recrystallization of Olivine During Simple Shear: Evolution of Microstructure and Crystallographic Preferred Orientation From Full‐Field Numerical Simulations

  2024cites this paper
• Enhanced structural analysis through a hybrid analogue-digital mapping approach: integrating field and UAV survey with microtomography to characterize metamorphic rocks

  2024cites this paper
• Quantification of grain boundary mobilities in natural olivine by annealing experiments and full-field modelling

  2024cites this paper
• Deformation and paleopiezometry of auriferous quartz veins in Archean orogenic gold deposits of the Abitibi greenstone belt

  2023cites this paper
• Melt-enhanced strain localization and phase mixing in a large-scale mantle shear zone (Ronda peridotite, Spain)

  2023cites this paper
• Dislocation theory of steady and transient creep of crystalline solids: Predictions for olivine

  2023cites this paper
• Dynamically recrystallized grains identified via the application of Gaussian mixture model to EBSD data

  2023cites this paper
• Some Like It Cold: The “Conundrum of Samail” Revisited

  2023cites this paper
• MYflow - A simple computer program for rheological modelling of mylonites

  2023cites this paper
• A process-based theory for subgrain-size and grain-size piezometry

  2023cites this paper
• Deformation behavior and fluid action of quartz veins in the Xuelongshan metamorphic complex, Western Yunnan

  2023cites this paper
• High Stress Deformation and Short‐Term Thermal Pulse Preserved in Pyroxene Microstructures From Exhumed Lower Crustal Seismogenic Faults (Lofoten, Norway)

  2022cites this paper
• Evaluating the distinct identity and the orogen-scale nature of the Munsiari thrust in the Himalaya

  2022cites this paper
• Shear zones in the southern Eyre Peninsula, South Australia: Quartz c-axis fabrics in granulite facies mylonitic orthogneisses and relationship to mafic dykes

  2022cites this paper
• Grain-size-evolution controls on lithospheric weakening during continental rifting

  2022cites this paper
• Prolonged grain boundary sliding in naturally deformed calcite marble at the middle crustal level

  2022cites this paper
• Rheology, shear zone width, microstructural evolution and tectonics of a zippered strike-slip shear zone: The Senador Pompeu shear zone, northern Borborema Province, Brazil

  2022cites this paper
• Contribution of deformation and reaction of amphiboles to the weakening of the middle continental crust: A case study from sheared diorites along the Shuiyu shear zone in Northern Beijing

  2022cites this paper
• Strain localization at brittle-ductile transition depths during Miocene magmatism and exhumation in the southern Basin and Range

  2022cites this paper
• Monazite as a monitor of shear strain in orogenic crust

  2022cites this paper
• The ≥6-km Cuesta de Randolfo mylonite zone in Ordovician Famatinian peraluminous granites, NW Argentina: Strain-localization as a function of protolith composition

  2021cites this paper
• The Cycladic Blueschist Unit of the Hellenic subduction orogen: Protracted high-pressure metamorphism, decompression and reimbrication of a diachronous nappe stack

  2021cites this paper
• Stress sensitivity of high-temperature microstructures in ice, with potential applications to quartz

  2021cites this paper
• Evolution of fluid pathways during eclogitization and their impact on formation and deformation of eclogite: A microstructural and petrological investigation at the type locality (Koralpe, Eastern Alps, Austria)

  2021cites this paper
• A natural example of brittle-to-viscous strain localization under constant-stress conditions: a case study of the Kellyland fault zone, Maine, USA

  2021cites this paper
• Structural and rheological features of the northeastern Sanyang shear zone in the eastern Jiangnan orogen: Indications for early Paleozoic orogeny in the South China block

  2021cites this paper
• Dissolution precipitation creep as a process for the strain localisation in mafic rocks

  2021cites this paper
• WHOLE-LITHOSPHERE SHEAR DURING OBLIQUE RIFTING

  2021cites this paper
• What controls the width of ductile shear zones

  2021cites this paper
• Self-Consistent Grain Size Evolution controls Strain Localization during Rifting

  2021cites this paper
• Heterogeneous material properties – as inferred from seismic attenuation - influenced multiple fault rupture and ductile creep of the Kaikoura Mw 7.8 earthquake, New Zealand

  2021cites this paper
• Oceanic transform fault seismicity and slip mode influenced by seawater infiltration

  2021cites this paper
• Interactions between deformation and dissolution-precipitation reactions in plagioclase feldspar at greenschist facies

  2021cites this paper
• The importance of tangential motion in the Central Alps: Kinematic analysis and Rb Sr dating of mylonitic rocks from the Pennine nappes in the eastern Central Alps

  2021cites this paper
• Natural and Experimental Constraints on a Flow Law for Dislocation‐Dominated Creep in Wet Quartz

  2021cites this paper
• Evolution of Microstructural Properties in Sheared Iron‐Rich Olivine

  2021cites this paper
• Experimental Plastic Reactivation of Pseudotachylyte‐Filled Shear Zones

  2021cites this paper
• The Deep Structure and Rheology of a Plate Boundary-Scale Shear Zone: Constraints from an Exhumed Caledonian Shear Zone, NW Scotland

  2020cites this paper
• Shear localization in metallic materials at high strain rates

  2020cites this paper
• Deformation Memory in the Lithosphere: A Comparison of Damage‐dependent Weakening and Grain‐Size Sensitive Rheologies

  2020influential citation
• Deformation memory in the lithosphere: A comparison of damage-dependent weakening and grain-size sensitive rheologies

  2020cites this paper
• Flow‐to‐Friction Transition in Simulated Calcite Gouge: Experiments and Microphysical Modeling

  2020cites this paper
• Quartz textural analysis from an anastomosing shear zone system: Implications for the tectonic evolution of the Ribeira belt, Brazil

  2020cites this paper
• Can Grain Size Reduction Initiate Transform Faults?—Insights From a 3‐D Numerical Study

  2020cites this paper
• The Capo Castello Shear Zone (Eastern Elba Island): Deformation at the Contact between Oceanic and Continent Tectonic Units

  2020cites this paper
• Rates of Olivine Grain Growth During Dynamic Recrystallization and Postdeformation Annealing

  2020influential citation
• Characterization of recovery onset by subgrain and grain boundary migration in experimentally deformed polycrystalline olivine

  2020cites this paper
• The effects of quartz Dauphiné twinning on strain localization in a mid-crustal shear zone

  2020cites this paper
• Dynamic recrystallization mechanisms and vorticity estimation of the Terrane Boundary Shear Zone (Lakhna shear zone): Implications on dynamics of juxtaposition of the Eastern Ghats Mobile Belt with the Bastar Craton, NW Odisha

  2020cites this paper
• The relative strengths of deforming mineral phase assemblages: Geometrically necessary deformation mechanisms

  2020cites this paper
• 2 D and 3 D simulation of grain growth in olivine aggregates using a full field model based on the level set method

  2019cites this paper
• Shear localisation in anisotropic, non-linear viscous materials that develop a CPO: A numerical study

  2019cites this paper
• The frequency-size scaling of non-volcanic tremors beneath the San Andreas Fault at Parkfield: Possible implications for seismic energy release

  2019cites this paper
• New Insights into the Position and Geometry of the Main Central Thrust from Sikkim, Eastern Himalaya

  2019cites this paper
• Fracturing and Formation of Ductile Shear Zones in the Continental Lower Crust

  2019cites this paper
• Deformation mechanisms in micas and mica-bearing mylonites in regional scale shear zones

  2019cites this paper
• From intracrystalline distortion to plate motion: Unifying structural, kinematic, and textural analysis in heterogeneous shear zones through crystallographic orientation-dispersion methods

  2019cites this paper
• Middle to Late Miocene Age for the End of Amphibolite‐Facies Mylonitization of the Alpine Schist, New Zealand: Implications for Onset of Transpression Across the Alpine Fault

  2019cites this paper
• Major shear zone within the Greater Himalayan Sequence and sequential evolution of the metamorphic core in Sikkim, India

  2019cites this paper
• In situ evidence of earthquakes near the crust mantle boundary initiated by mantle CO2 fluxing and reaction-driven strain softening

  2019cites this paper
• Crystallographic preferred orientations of plagioclase via grain boundary sliding in a lower-crustal anorthositic ultramylonite

  2019cites this paper
• Rates of Dynamic Recrystallization in Geologic Materials

  2019cites this paper
• Mechanisms of strain localisation in the lithosphere

  2019cites this paper
• On the Thermo-Mechanics of Ductile Strain Localization in the Lithosphere and New Steps towards a Nappe Theory of the Helvetic Alps

  2019cites this paper
• Weaker Than Weakest: On the Strength of Shear Zones

  2019cites this paper
• Spontaneous generation of ductile shear zones by thermal softening: Localization criterion, 1D to 3D modelling and application to the lithosphere

  2019cites this paper
• Deformation conditions during syn-convergent extension along the Cordillera Blanca shear zone, Peru

  2019cites this paper
• Time for anisotropy: The significance of mechanical anisotropy for the development of deformation structures

  2019cites this paper
• Preservation of high‐P rocks coupled to rock composition and the absence of metamorphic fluids

  2019cites this paper
• A cavitation-seal mechanism for ultramylonite formation in quartzofeldspathic rocks within the semi-brittle field (Vivero fault, NW Spain)

  2018cites this paper
• Active tectonics around the Yakutat indentor: New geomorphological constraints on the eastern Denali, Totschunda and Duke River Faults

  2018cites this paper
• New analogue materials for nonlinear lithosphere rheology, with an application to slab break-off

  2018cites this paper
• Comment on “Quartz grainsize evolution during dynamic recrystallization across a natural shear zone boundary” by Haoran Xia and John P. Platt

  2018cites this paper
• Quartz grainsize evolution during dynamic recrystallization across a natural shear zone boundary

  2018cites this paper
• Geochronology of shear zones – A review

  2018cites this paper
• Greenland Ice Sheet: Higher Nonlinearity of Ice Flow Significantly Reduces Estimated Basal Motion

  2018cites this paper
• Seismic cycle feedbacks in a mid-crustal shear zone

  2018cites this paper
• Development of sigmoidal en-échelon microfractures in beryl and the role of strain localization evidenced by fluid inclusions

  2018cites this paper
• Quantifying magnitudes of shear heating in metamorphic systems

  2018cites this paper
• High-temperature shear zone formation in Carrara marble: The effect of loading conditions

  2018cites this paper
• Deformation of Fine‐Grained Quartz Aggregates by Mixed Diffusion and Dislocation Creep

  2018cites this paper
• 2D and 3D simulation of grain growth in olivine aggregates using a full field model based on the level set method

  2018cites this paper