Mössbauer and Synchrotron MicroXANES Analysis of NWA2737

Physics

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Scientific paper

We report on the distribution of Fe3+ between the mineral phases in NWA
2737 as measured with Mössbauer and synchrotron microXANES
spectrometry. The brown olivine in NWA 2737 implies that it has been
subject to different processes than Chassigny.

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