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Updated: Dec 2, 2025

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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Greigite (Fe3S4) is thermodynamically stable: Implications for its terrestrial and planetary occurrence

Tamilarasan Subramani1, Kristina Lilova1, Mykola Abramchuk1

  • 1School of Molecular Sciences and Center for Materials of the Universe, Arizona State University, Tempe, AZ 85281.

Proceedings of the National Academy of Sciences of the United States of America
|November 3, 2020
PubMed

Keywords:
greigitehigh pressuremagnetismterrestrial planetsthermodynamic stability

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