Show simple item record

dc.contributor.authorColomer i Busquets, M.
dc.contributor.authorSantanach, P.
dc.date.accessioned2020-06-26T09:55:08Z
dc.date.available2020-06-26T09:55:08Z
dc.date.issued1988
dc.identifier.urihttp://hdl.handle.net/10272/18395
dc.description.abstractThe Calatayud-Daroca Basin is located in the Iberian Range. The SW margin of this Basin is the Jiloca fau/t. The evolution of the Basin during the Miocene, was conditioned by dextral slip on this fault. During the Pliocene the Jiloca fault had a normal slip, resulting in the Jiloca Basin formationes_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherThrustes_ES
dc.subject.otherStrike-slipes_ES
dc.subject.otherNeogenees_ES
dc.subject.otherCalatayud-Daroca Basines_ES
dc.titleEstructura y evolución del borde sur-occidental de la Fosa de Calatayud-Darocaes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


Files in this item

This item appears in the following Collection(s)

Show simple item record

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

Copyright © 2008-2010. ARIAS MONTANO. Repositorio Institucional de la Universidad de Huelva
Contact Us | Send Feedback |