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Deformation-induced trace element redistribution in zircon revealed using atom probe tomographyMessengers from the deep: Fossil wadsleyite-chromite microstructures from the Mantle Transition ZoneThe integration of experimental in-situ EBSD observations and numerical simulations: a novel technique of microstructural process analysis.Making EBSD on water ice routine.Hornblendite delineates zones of mass transfer through the lower crustDeformation-resembling microstructure created by fluid-mediated dissolution-precipitation reactionsSub-structure characterization of experimentally and naturally deformed ice using cryo-EBSD.Redox-freezing and nucleation of diamond via magnetite formation in the Earth's mantle.Evaluating the importance of metamorphism in the foundering of continental crust.The Weighted Burgers Vector: a new quantity for constraining dislocation densities and types using electron backscatter diffraction on 2D sections through crystalline materials.The importance of fracture-healing on the deformation of fluid-filled layered systemsTime for anisotropy: The significance of mechanical anisotropy for the development of deformation structuresSubgrain Rotation Recrystallization During Shearing: Insights From Full-Field Numerical Simulations of Halite PolycrystalsDetermining relative bulk viscosity of kilometre-scale crustal units using field observations and numerical modellingTrace element homogeneity from micron- to atomic scale: Implication for the suitability of the zircon GJ-1 as a trace element reference materialMaghemite soil nodules reveal the impact of fire on mineralogical and geochemical differentiation at the Earth’s surfaceRheology, microstructure and crystallographic preferred orientation of matrix containing a dispersed second phase: Insight from experimentally deformed iceCarbonado revisited: Insights from neutron diffraction, high resolution orientation mapping and numerical simulationsCoupled extrusion of sub-arc lithospheric mantle and lower crust during orogen collapse: a case study from Fiordland, New ZealandIn search of early life: Carbonate veins in Archean metamorphic rocks as potential hosts of biomarkersLocal partial melting of the lower crust triggered by hydration through melt-rock interaction: an example from Fiordland, New ZealandMass transfer in the lower crust: Evidence for incipient melt assisted flow along grain boundaries in the deep arc granulites of Fiordland, New ZealandShape of pinch and swell structures as a viscosity indicator: Application to lower crustal polyphase rocksStrain localization in polycrystalline material with second phase particles: Numerical modeling with application to ice mixturesSurface morphology and structural types of natural impact apographitic diamondsSymplectite formation in the presence of a reactive fluid: insights from hydrothermal experimentsThe Anita Peridotite, New Zealand: Ultra-depletion and Subtle Enrichment in Sub-arc MantlePinch and swell structures: evidence for strain localisation by brittle–viscous behaviour in the middle crustStrain localization in brittle–ductile shear zones: fluid-abundant vs. fluid-limited conditions (an example from Wyangala area, Australia)Effect of local stress heterogeneities on dislocation fields: Examples from transient creep in polycrystalline iceExperimental deformation of deuterated ice in 3D and 2D: identification of grain-scale processesFabric development during exhumation from ultrahigh-pressure in an eclogite-bearing shear zone, Western Gneiss Region, NorwayFluid-present deformation aids chemical modification of chromite: Insights from chromites from Golyamo Kamenyane, SE BulgariaOrthopyroxene–omphacite- and garnet–omphacite-bearing magmatic assemblages, Breaksea Orthogneiss, New Zealand: Oxidation state controlled by high-P oxide fractionationPink color in Type I diamonds: Is deformation twinning the cause?The effect of pre-tectonic reaction and annealing extent on behaviour during subsequent deformation: insights from paired shear zones in the lower crust of Fiordland, New ZealandThe influence of phase and grain size distribution on the dynamics of strain localization in polymineralic rocksSimulation of surface dynamics during dissolution as a function of the surface orientation: Implications for non-constant dissolution ratesDirect Observations of the Dissolution of Fluorite Surfaces with Different OrientationsImportance of surface structure on dissolution of fluorite: Implications for surface dynamics and dissolution rates
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