Unravelling the complex interaction between mantle and crustal magmas encoded in the lavas of San Vincenzo (Tuscany, Italy). Part I: Petrography and Thermobarometry
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文摘

Complex interaction between mantle-derived and crustal anatectic magmas

Rhyolites hosting magmatic enclaves, xenoliths, sialic and ultramafic cognates

Crystallization at both equilibrium and disequilibrium conditions

Crystallization in a large T range (710–1015 °C) at crustal depths (8–24 km)

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