Estructura alpina de los alrededores de Guadalix de la Sierra (S.E. del Sistema Central español) basada en interpretaciones gravimétricas

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dc.contributor.authorIzquierdo Revilla, F. J.
dc.contributor.authorCarbó Gorosabel, A.
dc.date.accessioned2017-07-19T10:14:10Z
dc.date.available2017-07-19T10:14:10Z
dc.date.issued1994
dc.description.abstractA detailed gravimetric study has been carried out in a sector in SE border of the Spanish Central Range (in the area of Guadalix de la Sierra) in which fractures have been detected that affect both the Hercian basement and the Mesozoic and Tertiary cover that put the several structural units existing in the area into contact. Two faults of N60º E and N75º E trend have acted as a low angle thrust, while one of N30- has a strike-slip reverse component and another norm al fault of a NiOO-E direction is also present. The origin of the faults Is in the Tardihercinian fractures which were prone to slipping durin the Alpine Orogenyes_ES
dc.identifier.urihttp://hdl.handle.net/10272/13940
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherSistema Central españoles_ES
dc.subject.otherGravity modelses_ES
dc.subject.otherAlpine tectonices_ES
dc.subject.otherTardihercinian faultinges_ES
dc.titleEstructura alpina de los alrededores de Guadalix de la Sierra (S.E. del Sistema Central español) basada en interpretaciones gravimétricases_ES
dc.titleAlpine structure in the area of Guadalix de la Sierra (S.E. of Spanish central range) based on gravimetric interpretationseng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 16, (1994)