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Autor Araña, V. |
Documentos disponibles escritos por este autor (5)
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Fernández, J. ; Romero, Rosana ; Carrasco, Daniel ; Tiampo, K. F. ; Rodríguez Velasco, Gema ; Aparicio, A. ; Araña, V. ; Gónzalez Matesanz, F. J. | Blackwell Publishing Ltd | 2005Tenerife is one of the most well monitored islands of the Canaries, but the surveillance generally is centred on Las Canadas Caldera, where the Teide volcano is located. In the last 180 000 yr, the eruptions on Tenerife Island have never occurre[...]texto impreso
Vieira, Ricardo ; Toro y Llaca, Carmen de ; Araña, V. | Instituto de Astronomía y Geodesia (IAG-CSIC-UCM) | 1986In this study, the first results obtained in a gravimetric exploration in the Caldera of Teide, Tenerife, Canary Islands, are presented. The gravimetric anomalies observed permit us to deduce the existence of a double vault, with an important ma[...]texto impreso
Araña, V. ; Camacho, A.G. ; Garcia, A. ; Montesinos, F. G. ; Blanco, I. ; Vieira, Ricardo ; Felpeto, A. | Elsevier Science Publishers | 2000Gravity and magnetic methods have been applied to the Tenerife Island, to provide new information about its internal structure. For this study, 365 gravity stations covering the central part of the island have been selected. The anomalous densit[...]texto impreso
Betancourt, N. ; Betancourt, N. ; Arias, C. ; Durán, F. ; Araña, V. | Institute of Physics Publishing | 2020-05-04T19:53:31ZIn the present study, an analysis of plain and reinforced concrete beams under monotonic loading was made based on the Fixed Smeared Crack approach. The objectives of this research were to analyze the nonlinear behavior of the selected cases of [...]texto impreso
Anguita, Francisco ; Araña, V. ; Barberi, F. ; Díez Gil, J. ; Ortiz, R. ; Sbrana, A. | Instituto Geológico y Minero de España (Madrid) | 1987La Formación Roque Nublo (F. R. N.) es un conjunto de materiales en el que predominan coladas lávicas y piroclásticas de edad pliocena, emitidas en un episodio eruptivo corto pero de intensidad extrema, en la isla de Gran Canaria. Con el present[...]