Phase Transition of FeO and Stratification in Earth’s Outer Core-Reference-Cited by-同舟云学术

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Phase Transition of FeO and Stratification in Earth’s Outer Core

Published:2011-11-11 Issue:6057 Volume:334 Page:792-794
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Ozawa Haruka¹²,Takahashi Futoshi²,Hirose Kei¹²,Ohishi Yasuo³,Hirao Naohisa³

Affiliation:

1. Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Kanagawa 237-0061, Japan.

2. Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo 152-8551, Japan.

3. Japan Synchrotron Radiation Research Institute, Sayo, Hyogo 679-5198, Japan.

Abstract

Stratified convection in the outer core may influence Earth’s magnetic field.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference34 articles.

1. Elasticity and constitution of the Earth's interior

2. Effect of light elements on the sound velocities in solid iron: Implications for the composition of Earth's core

3. Composition and temperature of the Earth’s core constrained by combining ab initio calculations and seismic data

4. In Situ Determination of the NiAs Phase of FeO at High Pressure and Temperature

5. Phase transition boundary between B1 and B8 structures of FeO up to 210GPa

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