Análisis de la fábrica magnética en el Sinclinorio de Bizkaia: Implicaciones en la tectónica regional

A combined structural and AMS analysis is made in Upper Cretaceous rocks from the periclinal closure of the Biscay Synclinorium (Basque-Cantabrian basin). Fieldwork has led to the recognition of a broad band with a pervasive foliation along the NE limb. The magnetic fabrics are grouped into two zone...

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Detalles Bibliográficos
Autores: Vegas, Néstor, Aranguren, A., Rodríguez, Lidia, Cuevas, Julia, Tubía, José María, Esteban, José Julián
Tipo de recurso: artículo
Fecha de publicación:2017
País:España
Institución:Universidad de Huelva (UHU)
Repositorio:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Idioma:español
OAI Identifier:oai:ariasmontano.uhu.es:10272/15139
Acceso en línea:http://hdl.handle.net/10272/15139
Access Level:acceso abierto
Palabra clave:Fábrica magnética
Sinclinorio de Bizkaia
Cuenca Vasco-Cantábrica
Zona de cizalla
Magnetic fabrics
Biscay Synclinorium
Basque-Cantabrian basin
Shear zone
Descripción
Sumario:A combined structural and AMS analysis is made in Upper Cretaceous rocks from the periclinal closure of the Biscay Synclinorium (Basque-Cantabrian basin). Fieldwork has led to the recognition of a broad band with a pervasive foliation along the NE limb. The magnetic fabrics are grouped into two zones: 1) the samples from the core record magnetic lineations coincident with the SO/S 1 intersection lineation that are parallel to the synclinorium axis, and 2) the magnetic lineations from the NE limb are orthogonal to the synclinorium axis and concentrate around the down-dip direction of S 1. This partitioning of magnetic fabrics suggests in creasing deformation from the core, characterised by mixed (sedimentary and tectonic) magnetic fabrics, to the northeastern limb, where tectonic fabrics prevail. Field data and magnetic fabrics are consistent with an unusually high deformation in the NE limb of the synclinorium, which could be associated with a hitherto unknown shear zone at regional scale. A top to the NE movement of the shear zone would explain the trend of the magnetic lineation in the northeastern limb of the Biscay Synclinorium