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Contributions to Mineralogy and Petrology(1)
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scopus(5)
Barium-rich fluids and melts in a subduction environment (La Corea and Sierra del Convento mélanges, eastern Cuba)
ArticleAbstract: Whole-rock compositions of muscovite-bearing amphibolite, trondhjemite, pegmatite and quartz-muscoviPalabras claves:Ba-rich fluid, Caribbean plate, eastern Cuba, Phengite, subduction channel, TrondhjemiteAutores:Blanco-Quintero I.F., García-Gasco A., Lázaro C., Proenza J.A., Yamirka Rojas-AgramonteFuentes:scopusAncient xenocrystic zircon in young volcanic rocks of the southern Lesser Antilles island arc
ArticleAbstract: The Lesser Antilles arc is one of the best global examples in which to examine the effects of the inPalabras claves:230 Th disequilibrium, Carriacou-Petite Martinique, Crustal assimilation, Grenada, Lesser Antilles, Zircon xenocrystAutores:Alfred Kron̈er, Arculus R., Buhre S., Echeverría C.M., García-Gasco A., Geng H., Jeffries T., Lázaro C., Mertz-Kraus R., Williams I.S., Wong J., Xie H., Yamirka Rojas-AgramonteFuentes:scopusCryptic alkaline magmatism in the oceanic Caribbean arc (Camagüey area, Cuba)
ArticleAbstract: Mid and Late Cretaceous arc-related basaltic rocks in the Camagüey area, East Central Cuba, record aPalabras claves:Caribbean island-arc, Cryptic hybridization, Island-arc magmas, phlogopiteAutores:Butjosa L., Cambeses A., García-Gasco A., Iturralde-Vinent M., Lázaro C., Piñero E., Proenza J.A., Torró L., Yamirka Rojas-AgramonteFuentes:scopusPartial melting and counterclockwise P-T path of subducted oceanic crust (Sierra del Convento Mélange, Cuba)
ArticleAbstract: Partial melting of subducted oceanic crust has been identified in the Sierra del Convento mélange (CPalabras claves:amphibolite, Cuba, Exhumation, Partial melting, Subduction, TrondhjemiteAutores:Alfred Kron̈er, Blanco-Quintero I.F., García-Gasco A., Lázaro C., Millán G., Neubauer F., Núñez K., Torres-Roldán R.L., Yamirka Rojas-AgramonteFuentes:scopusPetrogenesis of the Tampanchi Ultramafic–Mafic Complex (Ecuador): Geodynamic implications for the northwestern margin of South America during the late Cretaceous
ArticleAbstract: The Tampanchi Ultramafic–Mafic Complex (TUMC), located in the central segment of the Cordillera RealPalabras claves:arc magmatism, Cumulate texture, ECUADOR, Hydrous magma, Mafic intrusion, Northern andesAutores:Blanco-Quintero I.F., F. Villares, García-Gasco A., Lázaro C., Pedro S.B. Reyes, Proenza J.A., Rubén CartagenaFuentes:scopus