Articles | Volume 33, issue 3
https://doi.org/10.5194/ejm-33-249-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/ejm-33-249-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Review article
| 
03 May 2021
Review article |
| 03 May 2021
| 03 May 2021
Defects in olivine
Sylvie Demouchy
CORRESPONDING AUTHOR
Géosciences Montpellier, CNRS & Université de Montpellier,
Montpellier, 34095, France
Related authors
Sylvie Demouchy, Manuel Thieme, Fabrice Barou, Benoit Beausir, Vincent Taupin, and Patrick Cordier
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We report a comprehensive data set characterizing and quantifying two types of mineral defects in the most abundant mineral of Earth's upper mantle: olivine. Namely, we investigate translation defects of dislocation and rotation defects, called disclinations, in polycrystalline olivine deformed in uniaxial compression or torsion, at high temperature and pressure. The defects are identified via mapping of the crystallographic disorientation detected using electron backscatter diffraction.
Billy Clitton Nzogang, Manuel Thieme, Alexandre Mussi, Sylvie Demouchy, and Patrick Cordier
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Sylvie Demouchy, Manuel Thieme, Fabrice Barou, Benoit Beausir, Vincent Taupin, and Patrick Cordier
Eur. J. Mineral., 35, 219–242, https://doi.org/10.5194/ejm-35-219-2023, https://doi.org/10.5194/ejm-35-219-2023, 2023
Short summary
Short summary
We report a comprehensive data set characterizing and quantifying two types of mineral defects in the most abundant mineral of Earth's upper mantle: olivine. Namely, we investigate translation defects of dislocation and rotation defects, called disclinations, in polycrystalline olivine deformed in uniaxial compression or torsion, at high temperature and pressure. The defects are identified via mapping of the crystallographic disorientation detected using electron backscatter diffraction.
Billy Clitton Nzogang, Manuel Thieme, Alexandre Mussi, Sylvie Demouchy, and Patrick Cordier
Eur. J. Mineral., 32, 13–26, https://doi.org/10.5194/ejm-32-13-2020, https://doi.org/10.5194/ejm-32-13-2020, 2020
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Defects in minerals and phase transitions
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We sampled pyroclastic fallout deposits from Hungary and from New Zealand in order to get the original
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Partition coefficients are key to petrological modelling yet hard to estimate independently of measurements. Here we model the partitioning of Cr between garnet and clinopyroxene ab initio. Incorporation of Cr into crystal structures causes strain, and its energetic toll defines whether Cr favours one mineral or another. Comparing to Cr content in metamorphic rocks shows how mineral composition and structure set equilibrium partition coefficients and how kinetics hampers equilibrium.
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Short summary
Olivine, a ferromagnesian orthosilicate, is the most abundant mineral in Earth’s upper mantle but also in Mars' and Venus'. The olivine atomic structure is also used to manufacture lithium batteries. Like any other crystalline solid, olivine never occurs with a perfect crystalline structure: defects in various dimensions are ubiquitous. In this contribution, I review the current state of the art of defects in olivine and several implications for key processes in geodynamics.
Olivine, a ferromagnesian orthosilicate, is the most abundant mineral in Earth’s upper mantle...
