Información del autor
Autor Ibarrola, E. |
Documentos disponibles escritos por este autor (6)
Añadir el resultado a su cesta Hacer una sugerencia Refinar búsqueda
texto impreso
Ballcells, R. ; Barrera, José Luis ; Gómez, J.A. ; Cueto, L.A. ; Ancochea Soto, Eumenio ; Huertas Coronel, María José ; Ibarrola, E. ; Snelling, N. | Instituto Geológico y Minero de España (Madrid) | 1994Se han realizado once nuevas dataciones K-Ar de las coladas básicas (basaltos, nefelinitas) y sálicas (traquitas) de los tres edificios principales subaéreos (Tetir o Norte, Gran Tarajal o Central y Jandía o Sur) que constituyen la Fase miocena [...]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
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
We construct a Generalized p value for testing statistical hypotheses on the comparison of mean vectors in the sequential observation of two continuous time multidimensional Gaussian processes. The mean vectors depend linearly on two multidimens[...]texto impreso
Ibarrola, E. ; Fúster Casas , José María ; Ancochea Soto, Eumenio ; Huertas Coronel, María José | Sociedad Geológica de España | 1991-02A volcanic submarine formation crops out in the north coast of Tenerife, east of San Juan de la Rambla. This unit is formed by massive and pil/owed lavas, pillow-breccias, hyaloc/astites and palagonitic tuffs and is interpreted as consisUng of s[...]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[...]