Deformación de cizalla en el domo migmatítico de St. Malo (Macizo Armoricano, oeste de Francia)

Shear strain in the St. Malo migmatite dome (N Brittany)

dc.contributor.author	Román Berdiel, Teresa
dc.contributor.author	Gapais, D.
dc.contributor.author	Brun, J. P.
dc.date.accessioned	2015-05-08T11:39:09Z
dc.date.available	2015-05-08T11:39:09Z
dc.date.issued	1997
dc.identifier.uri	http://hdl.handle.net/10272/10534
dc.description.abstract	The Cadomian migmatite dome of St. Malo is affected by centimetric to metric shear bands. The shear bands bear a stretching lineation underlined by alignments of fibrous sillimanite crystals at Dinard and St. Briac outcrops. These shear bands were analysed by means of the Right Dihedra method. They indicate a NNE-SSW stretching direction and a subvertical shortening direction. They are consistent with foliation and stretching lineation orientations. This study suggests that the St. Malo migmatite dome was affected by a post-orogenic extensional tectonic regime	en_US
dc.language.iso	spa	en_US
dc.publisher	Sociedad Geológica de España	en_US
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Migmatites	en_US
dc.subject.other	Shear zone	en_US
dc.subject.other	Fault analysis	en_US
dc.subject.other	Cadomian orogeny	en_US
dc.subject.other	Armorican Massif	en_US
dc.title	Deformación de cizalla en el domo migmatítico de St. Malo (Macizo Armoricano, oeste de Francia)	en_US
dc.title	Shear strain in the St. Malo migmatite dome (N Brittany)	eng
dc.type	info:eu-repo/semantics/article	en_US
dc.rights.accessRights	info:eu-repo/semantics/openAccess	en_US

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

Shear strain in the St. Malo migmatite dome (N Brittany)

dc.contributor.author	Román Berdiel, Teresa
dc.contributor.author	Gapais, D.
dc.contributor.author	Brun, J. P.
dc.date.accessioned	2015-05-08T11:39:09Z
dc.date.available	2015-05-08T11:39:09Z
dc.date.issued	1997
dc.identifier.uri	http://hdl.handle.net/10272/10534
dc.description.abstract	The Cadomian migmatite dome of St. Malo is affected by centimetric to metric shear bands. The shear bands bear a stretching lineation underlined by alignments of fibrous sillimanite crystals at Dinard and St. Briac outcrops. These shear bands were analysed by means of the Right Dihedra method. They indicate a NNE-SSW stretching direction and a subvertical shortening direction. They are consistent with foliation and stretching lineation orientations. This study suggests that the St. Malo migmatite dome was affected by a post-orogenic extensional tectonic regime	en_US
dc.language.iso	spa	en_US
dc.publisher	Sociedad Geológica de España	en_US
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Migmatites	en_US
dc.subject.other	Shear zone	en_US
dc.subject.other	Fault analysis	en_US
dc.subject.other	Cadomian orogeny	en_US
dc.subject.other	Armorican Massif	en_US
dc.title	Deformación de cizalla en el domo migmatítico de St. Malo (Macizo Armoricano, oeste de Francia)	en_US
dc.title	Shear strain in the St. Malo migmatite dome (N Brittany)	eng
dc.type	info:eu-repo/semantics/article	en_US
dc.rights.accessRights	info:eu-repo/semantics/openAccess	en_US

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