Research ArticleGEODYNAMICS

Dislocation-accommodated grain boundary sliding as the major deformation mechanism of olivine in the Earth’s upper mantle

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Science Advances  02 Oct 2015:
Vol. 1, no. 9, e1500360
DOI: 10.1126/sciadv.1500360

Article Information

vol. 1 no. 9

Online ISSN: 
History: 
  • Received for publication March 20, 2015
  • Accepted for publication August 27, 2015

Author Information

  1. Tomohiro Ohuchi1,*,
  2. Takaaki Kawazoe1,2,
  3. Yuji Higo3,
  4. Ken-ichi Funakoshi3,4,
  5. Akio Suzuki5,
  6. Takumi Kikegawa6 and
  7. Tetsuo Irifune1,7
  1. 1Geodynamics Research Center, Ehime University, Matsuyama 790-8577, Japan.
  2. 2Bayerisches Geoinstitut, University of Bayreuth, 95440 Bayreuth, Germany.
  3. 3Japan Synchrotron Radiation Institute, Sayo, Hyogo 679-5198, Japan.
  4. 4Research Center for Neutron Science and Technology, Ibaraki 319-1906, Japan.
  5. 5Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan.
  6. 6Photon Factory, High Energy Accelerator Research Organization, Tsukuba 305-0801, Japan.
  7. 7Earth-Life Science Institute, Tokyo Institute of Technology, Tokyo 152-8550, Japan.
  1. *Corresponding author. E-mail: ohuchi{at}sci.ehime-u.ac.jp

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