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Title: Preferred Orientation of Quartz in Metamorphic Rocks from the Bergell Alps

Abstract

Crystal preferred orientation of 47 samples of quartzite and eight samples of associated marbles from the Bergell Alps have been analyzed with time-of-flight neutron diffraction and EBSD. The results show a clear distinction of texture types for quartzites transformed from Triassic sandstones and quartz layers in gneiss. Textures of Triassic quartzites are overall weak and display a maximum of c-axes perpendicular to the foliation or a crossed girdle perpendicular to the lineation. Pole figures for positive rhombs {10 $$\bar{1}$$ 1} show a maximum perpendicular to the foliation and negative rhombs {01$$\bar{1}$$ 1} generally display a minimum. Based on polycrystal plasticity models this texture type can be attributed to a combination of basal and rhombohedral slip. Asymmetry of the distributions is attributed to simple shear and local strain heterogeneities. The relatively weak texture is partially caused by muscovite limiting dislocation motion and grain growth, as well as adjacent layers of marble that accommodate significant strain. Most quartz layers in gneiss, including mylonites, display a texture with a-axes parallel to the lineation and a c-axis maximum in the intermediate fabric direction. This texture type can be attributed to dominant prismatic slip. Many samples are recrystallized and recrystallization appears to strengthen the deformation texture. The study shows good agreement of neutron diffraction and EBSD. Neutron diffraction data average over larger volumes and maximum pole densities are generally lower and more representative for the bulk material. With EBSD the microstructure and mechanical twinning can be quantified.

Authors:
ORCiD logo; ; ORCiD logo; ORCiD logo
Publication Date:
Research Org.:
Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
Sponsoring Org.:
USDOE
OSTI Identifier:
1529650
Alternate Identifier(s):
OSTI ID: 1558971
Report Number(s):
LA-UR-19-22182
Journal ID: ISSN 2075-163X; MBSIBI; PII: min9050277
Grant/Contract Number:  
FG02-05ER15637; 89233218CNA000001
Resource Type:
Published Article
Journal Name:
Minerals
Additional Journal Information:
Journal Name: Minerals Journal Volume: 9 Journal Issue: 5; Journal ID: ISSN 2075-163X
Publisher:
MDPI AG
Country of Publication:
Switzerland
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES

Citation Formats

Wenk, Hans-Rudolf, Yu, Rong, Vogel, Sven, and Vasin, Roman. Preferred Orientation of Quartz in Metamorphic Rocks from the Bergell Alps. Switzerland: N. p., 2019. Web. doi:10.3390/min9050277.
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Wenk, Hans-Rudolf, Yu, Rong, Vogel, Sven, & Vasin, Roman. Preferred Orientation of Quartz in Metamorphic Rocks from the Bergell Alps. Switzerland. https://doi.org/10.3390/min9050277
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Wenk, Hans-Rudolf, Yu, Rong, Vogel, Sven, and Vasin, Roman. Sun . "Preferred Orientation of Quartz in Metamorphic Rocks from the Bergell Alps". Switzerland. https://doi.org/10.3390/min9050277.
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@article{osti_1529650,
title = {Preferred Orientation of Quartz in Metamorphic Rocks from the Bergell Alps},
author = {Wenk, Hans-Rudolf and Yu, Rong and Vogel, Sven and Vasin, Roman},
abstractNote = {Crystal preferred orientation of 47 samples of quartzite and eight samples of associated marbles from the Bergell Alps have been analyzed with time-of-flight neutron diffraction and EBSD. The results show a clear distinction of texture types for quartzites transformed from Triassic sandstones and quartz layers in gneiss. Textures of Triassic quartzites are overall weak and display a maximum of c-axes perpendicular to the foliation or a crossed girdle perpendicular to the lineation. Pole figures for positive rhombs {10 $\bar{1}$ 1} show a maximum perpendicular to the foliation and negative rhombs {01$\bar{1}$ 1} generally display a minimum. Based on polycrystal plasticity models this texture type can be attributed to a combination of basal and rhombohedral slip. Asymmetry of the distributions is attributed to simple shear and local strain heterogeneities. The relatively weak texture is partially caused by muscovite limiting dislocation motion and grain growth, as well as adjacent layers of marble that accommodate significant strain. Most quartz layers in gneiss, including mylonites, display a texture with a-axes parallel to the lineation and a c-axis maximum in the intermediate fabric direction. This texture type can be attributed to dominant prismatic slip. Many samples are recrystallized and recrystallization appears to strengthen the deformation texture. The study shows good agreement of neutron diffraction and EBSD. Neutron diffraction data average over larger volumes and maximum pole densities are generally lower and more representative for the bulk material. With EBSD the microstructure and mechanical twinning can be quantified.},
doi = {10.3390/min9050277},
journal = {Minerals},
number = 5,
volume = 9,
place = {Switzerland},
year = {Sun May 05 00:00:00 EDT 2019},
month = {Sun May 05 00:00:00 EDT 2019}
}
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https://doi.org/10.3390/min9050277
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    Works referencing / citing this record:

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    journal, April 1986

    Entropy Optimization in Texture Goniometry. I. Methodology
    journal, July 1988

    Dauphiné twinning and texture memory in polycrystalline quartz. Part 3: texture memory during phase transformation
    journal, April 2009

    • Wenk, Hans-Rudolf; Barton, N.; Bortolotti, M.
    • Physics and Chemistry of Minerals, Vol. 36, Issue 10
    • DOI: 10.1007/s00269-009-0302-6

    The effect of Dauphiné twinning on plastic strain in quartz
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    • Menegon, Luca; Piazolo, Sandra; Pennacchioni, Giorgio
    • Contributions to Mineralogy and Petrology, Vol. 161, Issue 4
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    Quartz preferred orientation in naturally deformed mylonitic rocks (Montalto shear zone–Italy): a comparison of results by different techniques, their advantages and limitations
    journal, December 2016

    • Fazio, Eugenio; Punturo, Rosalda; Cirrincione, Rosolino
    • International Journal of Earth Sciences, Vol. 106, Issue 7
    • DOI: 10.1007/s00531-016-1424-y

    A self consistent approach of the large deformation polycrystal viscoplasticity
    journal, December 1987

    The effects of folding on the C-axis fabrics of a quartz mylonite
    journal, April 1977

    Preferred orientation of quartz produced by slip during plane strain
    journal, April 1977

    Geological significance of recovery and recrystallization processes in quartz
    journal, April 1977

    High temperature flow and dynamic recrystallization in carrara marble
    journal, June 1980

    Piezoelectric effects in quartz-rich rocks
    journal, August 1981

    Quartz textures from the Simplon Fault Zone, southwest Switzerland and north Italy
    journal, April 1987

    Fabric development in experimentally sheared quartzites
    journal, November 1989

    A new estimate of the conditions for transition from basal 〈a〉 to prism [c] slip in naturally deformed quartz
    journal, November 1995

    Fabric development in shear zones: theoretical controls and observed phenomena
    journal, January 1979

    The simulation of fabric development during plastic deformation and its application to quartzite: fabric transitions
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    Fabric transitions in the Saxony granulite terrain
    journal, January 1982

    Atypical textures in quartz veins from the Simplon Fault Zone
    journal, January 1987

    Pure shear and simple shear calcite textures. Comparison of experimental, theoretical and natural data
    journal, January 1987

    Simulation of fabric development in recrystallizing aggregates—I. Description of the model
    journal, January 1988

    Simulation of fabric development in recrystallizing aggregates—II. Example model runs
    journal, January 1988

    Simple shear deformation and quartz crystallographic fabrics: a possible natural example from the Torridon area of NW Scotland
    journal, January 1990

    The role of dynamic recrystallization in the development of lattice preferred orientations in experimentally deformed quartz aggregates
    journal, September 1993

    A self-consistent viscoplastic model: prediction of rolling textures of anisotropic polycrystals
    journal, February 1994

    Crystallographic preferred orientations and microstructure of a Variscan marble mylonite in the Ossa-Morena Zone (SW Iberia)
    journal, August 2007

    Effect of mica on the grain size of dynamically recrystallized quartz in a quartz–muscovite mylonite
    journal, December 2007

    Quartz fabrics in the Alpine Fault mylonites: Influence of pre-existing preferred orientations on fabric development during progressive uplift
    journal, May 2008

    • Toy, Virginia G.; Prior, David J.; Norris, Richard J.
    • Journal of Structural Geology, Vol. 30, Issue 5
    • DOI: 10.1016/j.jsg.2008.01.001

    Evolution of quartz microstructure and c-axis crystallographic preferred orientation within ductilely deformed granitoids (Arolla unit, Western Alps)
    journal, November 2008

    • Menegon, Luca; Pennacchioni, Giorgio; Heilbronner, Renee
    • Journal of Structural Geology, Vol. 30, Issue 11
    • DOI: 10.1016/j.jsg.2008.07.007

    Quartz microstructures and crystallographic preferred orientation: Which shear sense do they indicate?
    journal, October 2011

    • Kilian, Rüdiger; Heilbronner, Renée; Stünitz, Holger
    • Journal of Structural Geology, Vol. 33, Issue 10
    • DOI: 10.1016/j.jsg.2011.08.005

    The role of second phases for controlling microstructural evolution in polymineralic rocks: A review
    journal, December 2011

    Effect of pre-existing crystallographic preferred orientation on the rheology of Carrara marble
    journal, November 2014

    • de Raadt, Wilhelmina S.; Burlini, Luigi; Kunze, Karsten
    • Journal of Structural Geology, Vol. 68
    • DOI: 10.1016/j.jsg.2014.07.011

    Tracking mechanical Dauphiné twin evolution with applied stress in axial compression experiments on a low-grade metamorphic quartzite
    journal, July 2018

    Texture analysis with the new HIPPO TOF diffractometer
    journal, December 2003

    • Wenk, H. -R.; Lutterotti, L.; Vogel, S.
    • Nuclear Instruments and Methods in Physics Research Section A: Accelerators, Spectrometers, Detectors and Associated Equipment, Vol. 515, Issue 3
    • DOI: 10.1016/j.nima.2003.05.001

    Dynamic recrystallization near the brittle-plastic transition in naturally and experimentally deformed quartz aggregates
    journal, February 2008

    Fabric transitions in quartz via viscoplastic self-consistent modeling part I: Axial compression and simple shear under constant strain
    journal, December 2014

    The SKAT texture diffractometer at the pulsed reactor IBR-2 at Dubna: experimental layout and first measurements
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    • Nuclear Instruments and Methods in Physics Research Section A: Accelerators, Spectrometers, Detectors and Associated Equipment, Vol. 412, Issue 1
    • DOI: 10.1016/s0168-9002(98)00340-4

    Combined texture and structure analysis of deformed limestone from time-of-flight neutron diffraction spectra
    journal, January 1997

    • Lutterotti, L.; Matthies, S.; Wenk, H. -R.
    • Journal of Applied Physics, Vol. 81, Issue 2
    • DOI: 10.1063/1.364220

    Mechanical deformation of quartz: I. Constant strain-rate compression experiments
    journal, September 1970

    • Baëta, R. D.; Ashbee, K. H. G.
    • The Philosophical Magazine: A Journal of Theoretical Experimental and Applied Physics, Vol. 22, Issue 177
    • DOI: 10.1080/14786437008225847

    Theory of Preferred Crystal Orientation Developed by Crystallization under Stress
    journal, March 1959

    • Kamb, W. Barclay
    • The Journal of Geology, Vol. 67, Issue 2
    • DOI: 10.1086/626571

    Experimental Evidence of Basal Slip in Quartz
    journal, November 1964

    • Christie, J. M.; Griggs, D. T.; Carter, N. L.
    • The Journal of Geology, Vol. 72, Issue 6
    • DOI: 10.1086/627030

    X-Ray Analysis of Preferred Orientation in Fine-Grained Quartz Aggregates
    journal, March 1969

    • Baker, D. W.; Wenk, H. R.; Christie, J. M.
    • The Journal of Geology, Vol. 77, Issue 2
    • DOI: 10.1086/627419

    Shock metamorphism of quartz in nature and experiment: I. Basic observation and theory*
    journal, March 1994

    Distinction between amorphous and healed planar deformation features in shocked quartz using composite color scanning electron microscope cathodoluminescence (SEM-CL) imaging
    journal, October 2016

    • Hamers, Maartje F.; Pennock, Gill M.; Herwegh, Marco
    • Meteoritics & Planetary Science, Vol. 51, Issue 10
    • DOI: 10.1111/maps.12711

    Elastic constants of natural quartz
    journal, August 2003

    • Heyliger, Paul; Ledbetter, Hassel; Kim, Sudook
    • The Journal of the Acoustical Society of America, Vol. 114, Issue 2
    • DOI: 10.1121/1.1593063

    X-Ray Fabric Analysis of Hot-Worked and Annealed Flint
    journal, September 1967

    Quartz: Preferred Orientation in Rocks Produced by Dauphine Twinning
    journal, June 1970

    Analysis of crystallographic preferred orientations of experimentally deformed Black Hills Quartzite
    journal, January 2017

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