Show simple item record

Magnetic fabric of the doleritic dykes in the Panticosa pluton (Pyrenean Axial Zone)

dc.contributor.authorSantana, V.
dc.contributor.authorVegas, Néstor
dc.contributor.authorPinotti, Lucio P.
dc.contributor.authorTubía, José María
dc.description.abstractThis work deals with the magnetic fabrics of the doleritic dykes intruded in the Panticosa pluton. The dykes are grouped in two main families: one with N-S direction and another one E-W, the most common. The measured magnetic susceptibility values range from 390 10-6SI to 1464 10-6SI, being representative of paramagnetic rocks with a minor ferromagnetic component. The recorded magnetic foliations and lineations show a strong structural homogeneity all over the sampling transects. The obliquity between the magnetic foliations and lineations, and the walls of the dykes, implies that the magma was intruded taken advantage of an extensional process, oblique to the strike of the dykes. This process could be related with the regional stress field invoked to explain the intrusion of the Panticosa plutonen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.subject.otherDoleritic dykesen_US
dc.subject.otherMagnetic fabricen_US
dc.subject.otherPyrenean Axial Zoneen_US
dc.titleFábrica magnética de diques doleríticos del Plutón de Panticosa (Zona Axial, Pirineos)en_US
dc.titleMagnetic fabric of the doleritic dykes in the Panticosa pluton (Pyrenean Axial Zone)eng

Files in this item

This item appears in the following Collection(s)

Show simple item record

Atribución-NoComercial-SinDerivadas 3.0 España
Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España

Copyright © 2008-2010. ARIAS MONTANO. Repositorio Institucional de la Universidad de Huelva
Contact Us | Send Feedback |