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Sigmoid structures in the Hercynian Cauterets-Panticosa granité (Pyrenees)

dc.contributor.authorLeblanc, D.
dc.contributor.authorGleizes, Gérard
dc.contributor.authorSantana, V.
dc.contributor.authorOlivier, Phillippe
dc.contributor.authorBouchez, J. L.
dc.contributor.authorAranguren, A.
dc.date.accessioned2016-07-08T11:32:36Z
dc.date.available2016-07-08T11:32:36Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10272/12476
dc.description.abstractThe emplacement of the Cauterets-Panticosa granite massif (western Pyrenees) was controlled by dextral, 100° E-trending shear zones. The anisotropy of magnetic susceptibility allows us to obtain detailed structural maps of foliation trajectories and magmatic lineations of the Cauterets-Panticosa massif. Both types of structures draw large-scale sigmoid structures related to the dextral shear zonesen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherGranitesen_US
dc.subject.otherPyreneesen_US
dc.subject.otherMagnetic susceptibilityen_US
dc.titleEstructuras sigmoïdes en el macizo granítico hercínico de Cauterets-Panticosa (Pirineos)en_US
dc.titleSigmoid structures in the Hercynian Cauterets-Panticosa granité (Pyrenees)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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