English   español  
Por favor, use este identificador para citar o enlazar a este item: http://hdl.handle.net/10261/161077
COMPARTIR / IMPACTO:
Estadísticas
logo share SHARE   Add this article to your Mendeley library MendeleyBASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:
Título

Interacción agua-magma en la erupción del Volcán de Taco (Tenerife, I. Canarias)

AutorV. Araña; F. Bellido; Bustillo, Mª Ángeles ; R. Omarini; R. Ortiz
Palabras clavePiroclastos
Vulcanismo explosivo
Lapilli acrecional
Energia
Fecha de publicación1986
CitaciónAnales de Física. serie B, número especial, 82, 154- 175
ResumenThe Taco volcano (Tenerife) is a good example of water-magma interaction conditioned by its location in a coastal plane. This is an increasing interaction which, at the beginning of the eruption, takes material form in the way of rhythmical increments in the degree of pyroclast fragmentation, with short periods of high energy. The most sizeable processes of hydro-magmatic interaction develop during the terminal phase and the manifestations of explosive volcanism range from pyroclast falls to massive beds and accretional lapilli. The ejected materials have undergone a petrological and geochemical study, where special attention has been paid to accretional lapilli. An interaction model has finally been developed, calculating the energy associated to the various phases and the eruptive mechanisms.
URIhttp://hdl.handle.net/10261/161077
Aparece en las colecciones: (MNCN) Artículos
Ficheros en este ítem:
Fichero Descripción Tamaño Formato  
1986 Araña Bellido Bustillo Lapilli.pdf10,7 MBAdobe PDFVista previa
Visualizar/Abrir
Mostrar el registro completo
 


NOTA: Los ítems de Digital.CSIC están protegidos por copyright, con todos los derechos reservados, a menos que se indique lo contrario.