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Le Pico de Orizaba (Mexique): Structure et evolution d’un grand volcan andesitique complexe
ArticleAbstract: Volcan Pico de Orizaba, which marks the eastern end of the Trans-Mexican Volcanic Belt, is one of thPalabras claves:Autores:Cantagrel J.M., Claude RobinFuentes:scopusVolcan popocatepetl (Mexico): Structure, petrology and risks
ArticleAbstract: Volcan Popocatepetl, which lies 70 km southeast of Mexico City, is one of the most famous andesite cPalabras claves:Autores:Claude RobinFuentes:scopusRepetitive mixing events and holocene pyroclastic activity at Pico de Orizaba and Popocatepetl (Mexico)
ArticleAbstract: The Holocene volcanic activity which built up the present terminal cones of Pico de Orizaba and PopoPalabras claves:Autores:Cantagrel J.M., Claude Robin, Gourgaud A.Fuentes:scopusThe main stages of the evolution of an andesitic composite volcano: The nevado de toluca (Mexico)
ArticleAbstract: The Nevado de Toluca, in the middle of the Mexican volcanic belt, has been built by two very dissimiPalabras claves:Autores:Cantagrel J.M., Claude Robin, Vincent P.M.Fuentes:scopus