Abstract
In situ synchrotron X-ray powder diffraction measurements using a Paris-Edinburgh pressure cell were performed to investigate the nature of the high-pressure breakdown reaction of magnetite (Fe3O4). Refinement of diffraction patterns reveals that magnetite breaks down via a disproportionation reaction to Fe4O5 and hematite (Fe2O3) rather than undergoing an isochemical phase transition. This result, combined with literature data indicates (1) that this reaction occurs at ~9.5-11 GPa and 973-1673 K, and (2) these two phases should recombine at yet higher pressures to produce an h-Fe3O4 phase.
Received: 2012-6-20
Accepted: 2012-7-17
Published Online: 2015-4-2
Published in Print: 2012-10-1
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
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- Brittle-ductile microfabrics in naturally deformed zircon: Deformation mechanisms and consequences for U-Pb dating
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- Rates and mechanism of Y, REE, and Cr diffusion in garnet
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- Crystal chemistry of Bi- and Mn-bearing vesuvianite from Långban, Sweden
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