Abstract:The north and northwest margins of the Arabian plate are locus of a diffuse and long-lasting (early Miocene to Pleistocene) Na-alkali basaltic volcanism, sourced in the asthenosphere mantle. The occurrence and 20-Ma persistence of magma supply under the study area is explained considering that upwelling asthenosphere produces very limited magma volumes in the axial zone and portions of hot, fertile mantle continue their eastward migration and are stored at shallower depths under the 100-km thick Arabian lithos… Show more
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