Published March 23, 2020
| Version v2
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Melting curve and phase relations of Fe-Ni alloys at high pressure and high temperature: implications for the Earth core composition
Creators
- 1. European Synchrotron Radiation Facility, Grenoble, France
- 2. Institut de Mineralogie, de Physique des Materiaux, et de Cosmochimie (IMPMC), Sorbonne Universite - UPMC, UMR CNRS 7590, Museum National d'Histoire Naturelle, IRD UMR 206, F-75005, Paris, France
- 3. Graduate School of Advanced Science and Engineering, Hiroshima Univ., Higashi-Hiroshima, Japan
- 4. Institut for Fysik, Danmarks Tekniske Universitet, Kongens Lyngby, Denmark
- 5. Lawrence Livermore National Laboratory, Livermore, CA, USA
- 6. Geodynamics Research Center, Ehime University, Matsuyama, Japan
- 7. Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, IRD, IFSTTAR, ISTerre, 38000 Grenoble, France; Institut de Mineralogie, de Physique des Materiaux, et de Cosmochimie (IMPMC), Sorbonne Universite - UPMC, UMR CNRS 7590, Museum National d'Histoire Naturelle, IRD UMR 206, F-75005, Paris, France
Description
X-ray absorption data supporting results of the manuscript:
Melting curve and phase relations of Fe-Ni alloys at high pressure and high temperature: implications for the Earth core composition
submitted to Geophysical Research Letters