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Low Core-Mantle Boundary Temperature Inferred from the Solidus of Pyrolite

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Science  31 Jan 2014:
Vol. 343, Issue 6170, pp. 522-525
DOI: 10.1126/science.1248186

Article Information

vol. 343 no. 6170 522-525

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History: 
  • Received for publication November 6, 2013
  • Accepted for publication December 30, 2013

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Author Information

  1. Ryuichi Nomura1,*,
  2. Kei Hirose1,2,3,*,
  3. Kentaro Uesugi4,
  4. Yasuo Ohishi4,
  5. Akira Tsuchiyama5,
  6. Akira Miyake5,
  7. Yuichiro Ueno1,2
  1. 1Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo 152-8551, Japan.
  2. 2Earth-Life Science Institute, Tokyo Institute of Technology, Meguro, Tokyo 152-8551, Japan.
  3. 3Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Kanagawa 237-0061, Japan.
  4. 4Japan Synchrotron Radiation Research Institute, Sayo, Hyogo 679-5198, Japan.
  5. 5Division of Earth and Planetary Sciences, Kyoto University, Kyoto, Kyoto 606-8502, Japan.
  1. *Corresponding author. E-mail: nomura.r.ab{at}m.titech.ac.jp (R.N.); kei{at}elsi.jp (K.H.)

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