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The base of the Samail ophiolite is a metamorphic shear zone that provides key information about ophiolite emplacement. The classic exposure of this metamorphic sole at Wadi Tayin consists of a few meters of garnet-clinopyroxene mafic gneiss and 80 m of upper amphibolite facies mafic and quartzose tectonite, overlying 150 m of lower amphibolite facies mafic and sedimentary schist. The sole is bounded...
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