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Mylonite fabrics in Los Llanos Shear Zone (Calzadilla de los Barros, Badajoz)

dc.contributor.authorJiménez Díaz, Alberto
dc.contributor.authorCapote, Ramón
dc.contributor.authorTejero López, Rosa
dc.contributor.authorLunar, Rosario
dc.contributor.authorOrtega, Lorena
dc.contributor.authorMonterrubio, Serafín
dc.contributor.authorMaldonado, Casimiro
dc.contributor.authorRodríguez, David
dc.date.accessioned2014-04-25T12:10:24Z
dc.date.available2014-04-25T12:10:24Z
dc.date.issued2009
dc.identifier.urihttp://hdl.handle.net/10272/8050
dc.description.abstractThe Los Llanos Shear Zone bounds the Cabeza Gorda and Zafra units located in the Ossa-Morena Zone (SW Iberian Massif). Within the Cabeza Gorda unit two peridotitic massifs crop out, named Sierra Cabeza Gorda and Cerro Cabrera. The mylonitic rocks consist of metamorphic and peridotitic rocks extensively deformed that exhibit a penetrative foliation. Mylonitic fabrics are characterized by s and d structures and S-C and S-C’ band. Some examples show a crenulation cleavage that points out the existence of at least two deformation stages. Kinematic criteria are widespread, but dextral-reverse movement prevails both in outcrop and thin section. Los Llanos Shear Zone orientation is NW-SE, similar to variscan structures trend in the area, and deforms precambrian and paleozoic rocks. Los Llanos Shear Zone represents a dextral-reverse structure of Variscan ageen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherMylonitesen_US
dc.subject.otherPeridotitic massifsen_US
dc.subject.otherShear zoneen_US
dc.subject.otherCalzadilla de los Barrosen_US
dc.titleLa fábrica de las rocas miloníticas de la Zona de Cizalla de Los Llanos (Calzadilla de los Barros, Badajoz)en_US
dc.titleMylonite fabrics in Los Llanos Shear Zone (Calzadilla de los Barros, Badajoz)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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