Información del autor
Documentos disponibles escritos por este autor (9)
Añadir el resultado a su cesta Hacer una sugerencia Refinar búsqueda
texto impreso
Huertas Coronel, María José ; Arnaud, N. ; Ancochea Soto, Eumenio ; Cantagrel, Jean Marie ; Fúster Casas, José María | Elsevier Science Publishers | 2002-06-30Many felsic pyroclastic units of various types are exposed in different sectors of Tenerife. New 40Ar/39Ar determinations allow them to be placed more precisely in the general volcano-stratigraphic succession. According to geographic distributio[...]texto impreso
Se aportan datos que confirman que el metamorfismo del Guadarrama oriental corresponde al tipo distena-sillimanita, con un desarrollo zona1 que tiene grandes analogías con el trictaniorfismo barrowiense. Las zonas encontradas: cloritacloritoide-[...]texto impreso
Arnaud, N. ; Huertas Coronel, María José ; Cantagrel, Jean Marie ; Ancochea Soto, Eumenio ; Fúster Casas, José María | Sociedad Geológica de España | 2001-07During the evolution of the Las Cañadas volcanic edifice, debris avalanches were very significant destructive events. The Roques de Carcia unit was generated by such an evento 39Ar/40Ar dating has been carried out on different rock types related[...]texto impreso
Huertas Coronel, María José ; Ancochea Soto, Eumenio ; Cantagrel, Jean Marie ; Coello, Juan ; Fúster Casas, José María ; Ibarrola, E. | Sociedad Geológica de España | 1994-06Based on new radiometric data, a Pre-Cañadas volcanic building of 3.5-3.0 Ma has been defined. This new building is mainly compared of basaltic rack cropping out in several gorges to the S of Cañadas Building, inside of the «Pared de Las Cañadas[...]texto impreso
Arenas Martín, Ricardo ; Fúster Casas, José María ; González Lodeiro, F. ; Macaya, J. ; Martín Parra, L.M. ; Martínez Catalán, J.R. ; Villaseca González, Carlos | Sociedad Geológica de España | 1991La región de Segovia representa uno de los sectores más profundos de la Sierra de Guadarrama, donde el metamorfismo regional hercínico alcanza la mayor intensidad. La evolución tectonometamórfica de este sector coincide con la que se encuentra e[...]texto impreso
Ancochea Soto, Eumenio ; Huertas Coronel, María José ; Cantagrel, Jean Marie ; Coello, Juan ; Fúster Casas, José María ; Arnaud, N. ; Ibarrola, E. | Elsevier Science Publishers | 1999-02The volcano-stratigraphic and geochronologic data presented in this work show that the Tenerife central zone has been occupied during the last 3 Ma by shield or central composite volcanoes which reached more than 3000 m in height. The last volca[...]texto impreso
Ancochea Soto, Eumenio ; Fúster Casas, José María ; Ibarrola, Elisa ; Cendrero, Antonio | Elsevier | 1992New age determinations from Tenerife, together with those previously published (93 in all), provide a fairly comprehensive picture of the volcanic evolution of the island. The oldest volcanic series, with ages starting in the late Miocene, are f[...]texto impreso
Cantagrel, Jean Marie ; Arnaud, Nicolas O. ; Ancochea Soto, Eumenio ; Fúster Casas, José María ; Huertas Coronel, María José | Geological Society of America | 1999Geologic evidence on Tenerife, Canary Islands, indicates six successive north-directed debris avalanche events, including: the Anaga and Teno (ca. 6 Ma) events that affected the old basaltic series, and the Tigaiga (> 2.3 Ma), Roques de García ([...]texto impreso
Ancochea Soto, Eumenio ; Fúster Casas, José María ; Ibarrola, E. ; Cendrero, Antonio ; Coello, Juan ; Hernán, F. ; Cantagrel, Jean Marie ; Jamond, Colette | Elsevier Science Publishers | 1990-12-30New age determinations from Tenerife, together with those previously published (93 in all), provide a fairly comprehensive picture of the volcanic evolution of the island. The oldest volcanic series, with ages starting in the late Miocene, are f[...]
