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  • Quaternary Alkaline Basaltic Magmatism in the Saraijugh Area, Sanandaj–Sirjan Zone: Evidence for Low-Degree Partial Melting of the Lithospheric Mantle and Multistage Magmatic Evolution Based on Whole-Rock Geochemistry and Clinopyroxene Chemistry

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Manuscript ID : geology-55376 Visit : 1 Page: 61 - 81

Article Type: Original Research

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