Phase relations in iron-rich systems and implications for the Earth's core

Author:

Anderson William W.,Svendsen Bob,Ahrens Thomas J.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference48 articles.

1. Pyrite: shock compression, isentropic release, and composition of the Earth's core;Ahrens;J. Geophys. Res.,1987

2. A universal thermal equation of state;Anderson;J. Geodyn.,1984

3. Melting of iron sulfide and iron oxide at high pressure;Anderson;Lunar Planet. Sci.,1987

4. Melting in the FeFeS system and its relation to the compositions of the core of Earth and Mars;Anderson;Lunar Planet. Sci.,1987

5. Equation of state of the alpha and epsilon phases of iron;Andrews;J. Phys. Chem. Solids,1973

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1. Some Properties of the Fe-H System at High Pressures and Temperatures, and their Implications for the Earth's Core;High-Pressure Research: Application to Earth and Planetary Sciences;2013-03-18

2. Observation of O_2 inside voids formed in GeO_2 glass by tightly-focused fs-laser pulses;Optical Materials Express;2011-09-28

3. Evidence of superdense aluminium synthesized by ultrafast microexplosion;Nature Communications;2011-08-23

4. Iron – Oxygen – Silicon;Iron Systems, Part 5;2009

5. Sulfur in the Earth’s inner core;Earth and Planetary Science Letters;2001-12

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