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dc.contributor.authorAracil Ávila, E.
dc.contributor.authorVilas, Lorenzo
dc.date.accessioned2020-07-03T14:19:18Z
dc.date.available2020-07-03T14:19:18Z
dc.date.issued1987
dc.identifier.urihttp://hdl.handle.net/10272/18422
dc.description.abstractThe Mesozoic basement of Los Llanos de Albacete Tertiary Basin shows a fracture grid with two main orientations, almost orthogonal: NE-SW orientation is preferential, causing the basement to be divided in several blocks, limited by lystric faults and divided in smaller structures tilted to the NE. The Neogene filling of the basin is not affected by these fau/ts. The results have been obtained during the study of several wellses_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.otherJurassices_ES
dc.subject.otherCretaceouses_ES
dc.subject.otherFracturationes_ES
dc.subject.otherAutomatic-mappinges_ES
dc.subject.otherAlbacetees_ES
dc.titleEstructuración del basamento mesozoico en Los Llanos de Albacetees_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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Atribución-NoComercial-SinDerivadas 3.0 España
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