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Peridotites and wherlites with original characteristics in the transition zone of the semall ophiolite (OMAN). Implications concerning the partial melting dynamics of the mantle at oceanic ridges

M. Regba, M. Loubet

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Key concepts: Ophiolite, Geology, Partial melting, Transition zone, Mantle (geology), Geochemistry, Mid-ocean ridge, Oceanic crust

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Peridotites and wherlites with original characteristics in the transition zone of the semall ophiolite (OMAN). Implications concerning the partial melting dynamics of the mantle at oceanic ridges — Research Paper | ScholarLens