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This page is a summary of: Extreme geochemical variability through the dunitic transition zone of the Oman ophiolite: Implications for melt/fluid-rock reactions at Moho level beneath oceanic spreading centers, Geochimica et Cosmochimica Acta, August 2018, Elsevier,
DOI: 10.1016/j.gca.2018.05.012.
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