Abstract: Internally resistive heated diamond anvil cell experiments on Fe-Ni-Si alloy to 200 GPa and 3900 K and its implications for Earth's core (AGU Fall Meeting 2018)

Internally resistive heated diamond anvil cell experiments on Fe-Ni-Si alloy to 200 GPa and 3900 K and its implications for Earth's core

Tetsuya Komabayashi¹, Giacomo Pesce², Ryosuke Sinmyo³, Takaaki Kawazoe⁴, Helene Breton⁵, Yuta Shimoyama⁶, Konstantin Glazyrin⁷, Zuzana Konopkova⁷ and Mohamed Mezouar⁸, (1)University of Edinburgh, School of GeoSciences, Edinburgh, EH9, United Kingdom, (2)University of Edinburgh, Edinburgh, United Kingdom, (3)University of Tokyo, Bunkyo-ku, Japan, (4)University of Bayreuth, Bayerisches Geoinstitut, Bayreuth, Germany, (5)University of Edinburgh, School of GeoSciences, Edinburgh, United Kingdom, (6)Osaka University, Osaka, Japan, (7)DESY Deutsches Elektronen Synchrotron, Hamburg, Germany, (8)ESRF European Synchrotron Radiation Facility, Grenoble, France

Back to: Composition and Material Properties of the Core II Posters