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Modelling crust in the area of confluence of the Ibérica and Beticas chains obtained trough gravimetric data

dc.contributor.authorCastaño Fernández, Santiago
dc.contributor.authorCarbó Gorosabel, A.
dc.date.accessioned2017-06-12T08:52:51Z
dc.date.available2017-06-12T08:52:51Z
dc.date.issued1994
dc.identifier.urihttp://hdl.handle.net/10272/13796
dc.description.abstractThe results of a gravimetric reseach carried out in the SE of the Iberian Peninsula (areas of Albacete , Valencia and Murcia) allow us to obtain a pattern of the earth's modelling crust, in which the existence of a cortical slimming separating the iberica and Betica chain is observed. This is probably related to arifting process of the SW branch of the triple point of the Valencia basinen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherGravityen_US
dc.subject.otherModelling crusten_US
dc.subject.otherSE Spainen_US
dc.titleModelización de la corteza terrestre en la zona de confluencia de las cordilleras Ibérica y Béticas en base a datos gravimétricosen_US
dc.titleModelling crust in the area of confluence of the Ibérica and Beticas chains obtained trough gravimetric dataeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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