The High-Pressure Structural Evolution of Olivine along the Forsterite–Fayalite Join
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DOI: 10.3390/min9120790
Abstract: Structural refinements from single-crystal X-ray diffraction data are reported for olivine with a composition of Fo100 (forsterite Mg2SiO4, synthetic), Fo80 and Fo62 (~Mg1.6Fe0.4SiO4 and ~Mg1.24Fe0.76SiO4, both natural) at room temperature and high pressure to ~8… read more here.
Keywords: evolution olivine; olivine along; structural evolution; high pressure ... See more keywords