The dislocation-structure and crystallite-size in forsterite (olivine) deformed at 1400°C by 11 GPa

Krisztián Nyilas, Hélène Couvy, Patrick Cordier, Tamás Ungár

Research output: Contribution to journalArticle

2 Citations (Scopus)

Abstract

Synthetic forsterite samples were shear-deformed at 11 GPa, 1400°C in the multianvil apparatus. The deformation microstructures have been characterised by x-ray diffraction peak broadening and strain anisotropy analysis. The evolution of strain and stress are characterised as a function of the time duration of the high-pressure, high-temperature experiments.

Original languageEnglish
Pages (from-to)135-140
Number of pages6
JournalZeitschrift fur Kristallographie, Supplement
Volume1
Issue number23
DOIs
Publication statusPublished - Jan 1 2006

Keywords

  • Dislocation structure
  • Forsterite
  • High-pressure
  • High-temperature

ASJC Scopus subject areas

  • Materials Science(all)
  • Condensed Matter Physics
  • Inorganic Chemistry

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