Thermal equation of state of Fe3O4 magnetite up to 16 GPa and 1100 K

Abstract

Fe3O4 magnetite is an important mineral commonly found in various geological settings, including the planet Mars, whose thermo-elastic properties at high pressure and temperature are still poorly constrained. We performed X-ray diffraction measurements on natural This is the peer-reviewed, final accepted version for American Mineralogist, published by the Mineralogical Society of America.The published version is subject to change. Cite as Authors (Year) Title. American Mineralogist, in press.