In situ strength measurements on natural upper-mantle minerals

Junji Yamamoto, Jun Ichi Ando, Hiroyuki Kagi, Toru Inoue, Akihiro Yamada, Daisuke Yamazaki, Tetsuo Irifune

Research output: Contribution to journalArticle

31 Citations (Scopus)

Abstract

Using in situ strength measurements at pressures up to 10 GPa and at room temperature, 400, 600, and 700°C, we examined rheological properties of olivine, orthopyroxene, and chromian-spinel contained in a mantle-derived xenolith. Mineral strengths were estimated using widths of X-ray diffraction peaks as a function of pressure, temperature, and time. Differential stresses of all minerals increase with increasing pressure, but they decrease with increasing temperature because of elastic strain on compression and stress relaxation during heating. During compression at room temperature, all minerals deform plastically at differential stress of 4-6 GPa. During subsequent heating, thermally induced yielding is observed in olivine at 600°C. Neither orthopyroxene nor spinel shows complete stress relaxation, but both retain some stress even at 700°C. The strength of the minerals decreases in the order of chromian-spinel ≈ orthopyroxene > olivine for these conditions. This order of strength is consistent with the residual pressure of fluid inclusions in mantle xenoliths.

Original languageEnglish
Pages (from-to)249-257
Number of pages9
JournalPhysics and Chemistry of Minerals
Volume35
Issue number5
DOIs
Publication statusPublished - Jun 1 2008

Keywords

  • Fluid inclusion
  • Geobarometry
  • Mantle mineral
  • Rheology
  • X-ray diffraction measurement

ASJC Scopus subject areas

  • Materials Science(all)
  • Geochemistry and Petrology

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    Yamamoto, J., Ando, J. I., Kagi, H., Inoue, T., Yamada, A., Yamazaki, D., & Irifune, T. (2008). In situ strength measurements on natural upper-mantle minerals. Physics and Chemistry of Minerals, 35(5), 249-257. https://doi.org/10.1007/s00269-008-0218-6