Abstract
We have investigated the high-pressure behavior of Fe3O4 by in situ X-ray diffraction measurements from 11 to 103 GPa. Up to 70 GPa, the previous observed high-pressure Fe3O4 phase (h-Fe3O4) is stable, with a CaTi2O4-type structure. The compression curve shows an abnormal volume contraction at about 50 GPa, likely associated with the magnetic moment collapse observed at that pressure. Fitting the compression data up to 45 GPa to the Birch-Murnaghan equation of state yields a bulk modulus, KT0 = 172 GPa, and V0 = 277 Å3, with fixed Kʹ = 4. At a pressure between 64 and 73 GPa, a new structural transition was observed in Fe3O4, which can be attributed to a martensitic transformation as described by Yamanaka et al. (2008) for post-spinel structural transition. The diffraction data can be best fitted with a Pnma space group. No breakdown of Fe3O4 was observed up to at least 103 GPa. The new high-pressure polymorph is about 6% denser than the h-Fe3O4 phase at 75 GPa.
Acknowledgments
This work was supported by NSF geophysics grant to Y.F. and by the Carnegie Institution of Washington. We thank V. Prakapenka and P. Dera for technical assistance and C. Seagle for collecting part of the experimental data. The X-ray diffraction data were collected at APS GSECARS beamline supported by NSF, DOE, and the State of Illinois.
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Manuscript handled by Lars Ehm.
© 2016 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- Editorial
- The most-cited journal in mineralogy and petrology (and what scientists can learn from baseball)
- Fluids in the Crust
- Fluids in the crust during regional metamorphism: Forty years in the Waterville limestone
- Research Article
- Remanent magnetization, magnetic coupling, and interface ionic configurations of intergrown rhombohedral and cubic Fe-Ti oxides: A short survey
- Research Article
- Are covalent bonds really directed?
- Dana Medal Paper
- Constraints on the early delivery and fractionation of Earth’s major volatiles from C/H, C/N, and C/S ratios
- Crossroads in Earth and Planetary Materials
- Octahedral chemistry of 2:1 clay minerals and hydroxyl band position in the near-infrared: Application to Mars
- Special Collection: Advances in Ultrahigh-Pressure Metamorphism
- Multi-stage barite crystallization in partially melted UHP eclogite from the Sulu belt, China
- Spinels Renaissance: The Past, Present, and Future of those Ubiquitous Minerals and Materials
- Crystal chemistry of spinels in the system MgAl2O4-MgV2O4-Mg2VO4
- Spinels Renaissance: The Past, Present, and Future of those Ubiquitous Minerals and Materials
- Magnetite spherules in pyroclastic iron ore at El Laco, Chile
- Special Collection: Apatite: A Common Mineral, Uncommonly Versatile
- Evidence for dissolution-reprecipitation of apatite and preferential LREE mobility in carbonatite-derived late-stage hydrothermal processes
- Special Collection: Apatite: A Common Mineral, Uncommonly Versatile
- Compositional variation of apatite from rift-related alkaline igneous rocks of the Gardar Province, South Greenland
- Special Collection: Perspectives on Origins and Evolution of Crustal Magmas
- Dynamics and thermodynamics of magma mixing: Insights from a simple exploratory model
- Special Collection: From Magmas to Ore Deposits
- Geochemistry, petrologic evolution, and ore deposits of the Miocene Bodie Hills Volcanic Field, California and Nevada
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- Recognizing sulfate and phosphate complexes chemisorbed onto nanophase weathering products on Mars using in-situ and remote observations
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