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High-pressure behavior of Fe3P and the role of phosphorus in planetary cores

Earth and Planetary Science Letters, no. null (2014): 296-303

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Abstract

Fe3P is a candidate component in planetary cores. We have investigated high-pressure behavior of Fe3P by first-principles calculations and synchrotron X-ray diffraction. Theoretical calculations reveal a magnetic collapse at 40–65 GPa, accompanied by a structural transition. The possible high-pressure polymorph is either a distorted cemen...More

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