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The Variscan appinites from the San Martin del Pimpollar intrusion (Avila Batholith, Central Iberia) display geochemical and mineralogical evidence for hybridization with crustal-derived, partially molten, granodiorites and for rapid crystallization of residual melts.Quenching, apparently induced by the thermal contrast between mixing magmas, caused crystallization of hollow microphenocrysts of labradorite–bytownite,...
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