Mechanisms of transformation and deformation in Mg1.8Fe0.2SiO4 olivine and wadsleyite under non-hydrostatic stress

Catherine Dupas-Bruzek, Thomas Sharp, David C. Rubie, William B. Durham

Research output: Contribution to journalArticle

42 Scopus citations

Abstract

We have studied the effect of non-hydrostatic stress on the mechanisms of the olivine - wadsleyite-ringwoodite (α-β-γ) phase transformations and deformation mechanisms of olivine and wadsleyite at high pressure. Experiments were performed at 900°C in the β-stability field (15 GPa) for 0.5 h and in the β + γ stability field (16 GPa) for 11 h using a multianvil apparatus with San Carlos olivine as the starting material. A sample assembly designed to produce non-hydrostatic stress was used. The deformed samples have been characterised using optical and transmission electron microscopy. Remnant olivine contains high densities of mostly χ dislocations and deformation occurs by dislocation glide involving the slip systems (010)[001] and (100)[001]. In wadsleyite, dislocations are in a climb configuration, which suggests that self diffusion of Si and/or O is much faster in wadsleyite than in olivine at ~900°C. Wadsleyite also contains (010)β stacking faults which are interpreted to be growth defects that anneal out with time. During the olivine-wadsleyite transformation, non-hydrostatic stress results in anisotropic reaction textures. Wadsleyite nucleates preferentially on olivine grain boundaries that are oriented at a high angle to the direction of principal compressive stress and/or the growth of wadsleyite occurs preferentially in this direction. Wadsleyite transforms to ringwoodite by two competing mechanisms: 1) coherent intracrystalline nucleation on α dislocations, probably where they intersect (010)β stacking faults, and 2) partially-coherent nucleation at wadsleyite grain boundaries. Non-hydrostatic stress enhances transformation rates by increasing the density of dislocations which act as nucleation sites for ringwoodite. Although the samples were partially reacted under non-hydrostatic stress, there is no evidence for transformational faulting.

Original languageEnglish (US)
Pages (from-to)33-48
Number of pages16
JournalPhysics of the Earth and Planetary Interiors
Volume108
Issue number1
DOIs
StatePublished - May 29 1998

ASJC Scopus subject areas

  • Astronomy and Astrophysics
  • Geophysics
  • Physics and Astronomy (miscellaneous)
  • Space and Planetary Science

Fingerprint Dive into the research topics of 'Mechanisms of transformation and deformation in Mg<sub>1.8</sub>Fe<sub>0.2</sub>SiO<sub>4</sub> olivine and wadsleyite under non-hydrostatic stress'. Together they form a unique fingerprint.

  • Cite this