Supplemental material
Polar Research
Volume 35, 2016 - Issue 1
Related Research Data
Atypical textures in quartz veins from the Simplon Fault Zone
Source:
Elsevier BV
Two distinct Late Mesoproterozoic/Early Neoproterozoic basement provinces in central/eastern Dronning Maud Land, East Antarctica: The missing link, 15–21° E
Source:
Elsevier BV
U-Pb zircon age and Nd isotopic composition of granitoids, charnockites and supracrustal rocks from Heimefrontfjella, Antarctica
Source:
Springer Science and Business Media LLC
Simple shear deformation and quartz crystallographic fabrics: a possible natural example from the Torridon area of NW Scotland
Source:
Elsevier BV
Accretion and indentation tectonics at the southern edge of the Kaapvaal craton during the Kibaran (Grenville) orogeny
Source:
Geological Society of America
Determination and interpretation of preferred orientation with texture goniometry: An application of indicators to maximum entropy pole- to orientation-density inversion
Source:
Springer Science and Business Media LLC
Prism- and basal-plane parallel subgrain boundaries in quartz: a microstructural geothermobarometer
Source:
Wiley
Simulation of fabric development in recrystallizing aggregates—I. Description of the model
Source:
Elsevier BV
Einführung in die Gefügekunde der Geologischen Körper
Source:
Springer Vienna
A fracture model for quartz ribbons in straight gneisses
Source:
Elsevier BV
The eastern Tonale fault zone: a ‘natural laboratory’ for crystal plastic deformation of quartz over a temperature range from 250 to 700 °C
Source:
Elsevier BV
Microstructures in feldspars from a major crustal thrust zone: The Grenville Front, Ontario, Canada
Source:
Elsevier BV
Microstructures and Preferred Orientations of Experimentally Deformed Quartzites
Source:
Geological Society of America
Plastic-deformati on mechanisms in quartz: The effect of water
Source:
Elsevier BV
Tectonic interpretations of systematic variations in quartz c-axis fabrics across the Thompson Belt
Source:
Elsevier BV
Fabric transitions in the Saxony granulite terrain
Source:
Elsevier BV
The effect of the basal-prism mechanism switch on fabric development during plastic deformation of quartzite
Source:
Elsevier BV
The simulation of fabric development during plastic deformation and its application to quartzite: the influence of deformation history
Source:
Elsevier BV
18 – Preferred Orientations in Quartzites
Source:
Elsevier
S-C Mylonites
Source:
Elsevier BV
Dislocation creep regimes in quartz aggregates
Source:
Elsevier BV
A model for the development of a domainal quartz c-axis fabric in a coarse-grained gneiss
Source:
Elsevier BV
Mafic Dykes from Heimefrontfjella and implications for the post- Grenvillian to pre-Pan-African geological evolution of western Dronning Maud Land, Antarctica
Source:
Cambridge University Press (CUP)
Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican Shear Zone
Source:
HAL CCSD
Grenville-Age versus Pan-African Magnetic Anomaly Imprints in Western Dronning Maud Land, East Antarctica
Source:
University of Chicago Press
Quartz fabrics in the Alpine Fault mylonites: Influence of pre-existing preferred orientations on fabric development during progressive uplift
Source:
Elsevier BV
Le quartz en rubans dans les mylonites
Source:
EDP Sciences
The Effects of Strain on the Microstructures, Fabrics, and Deformation Mechanisms in Quartzites
Source:
The Royal Society
Quartz ribbons in high grade granite gneiss; modifications of dynamically formed quartz c-axis preferred orientation by oriented grain growth
Source:
Elsevier BV
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