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The extent of penetrative Pyrenean deformation in the Ebro foreland Basin: Magnetic fabric data from the eastern sector

We studied Cenozoic sedimentary rocks in the NE Ebro foreland Basin using the Anisotropy of Magnetic Susceptibility (AMS) as a proxy for grain preferred orientation. Our new data, in combination with existing results, reveal that penetrative strain by layer-parallel shortening extends well beyond th...

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Dades bibliogràfiques
Publicat a:Geologica Acta: an international earth science journal
Autors principals: J.M. Parés, D. Anastasio
Format: Artigo
Idioma:Inglês
Publicat: Universitat de Barcelona 2018
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Accés en línia:https://www.redalyc.org/articulo.oa?id=50559030003
https://www.redalyc.org/journal/505/50559030003/
https://www.redalyc.org/journal/505/50559030003/html/
https://www.redalyc.org/journal/505/50559030003/50559030003.epub
https://www.redalyc.org/journal/505/50559030003/movil
https://doi.org/10.1344/GeologicaActa2018.16.4.3
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