Análisis de la fracturación en la cuenca cenozoica de As Pontes (La Coruña)

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dc.contributor.authorFerrús, B.
dc.contributor.authorSantanach, P.
dc.date.accessioned2018-03-07T13:29:08Z
dc.date.available2018-03-07T13:29:08Z
dc.date.issued1994
dc.description.abstractMinor fault analysis using Angelier and Mechler (1977) and Etchecopar et al. (1981) methods have been carried out in the Cenozoic As Pontes Basin (NW Spain).The paleostress tensors obtained are in agreement with the deformation fie ld defined by large scale faults. The orientations of a 1 and a 3 are parallel to those of the regional shortening (N-S to NNW-SSE) and extension (E-W to ESE-WNW) directionses_ES
dc.identifier.urihttp://hdl.handle.net/10272/14409
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.otherNW Spaines_ES
dc.subject.otherCenozoices_ES
dc.subject.otherStrike-slip basines_ES
dc.subject.otherFault analysises_ES
dc.subject.otherStress fieldes_ES
dc.titleAnálisis de la fracturación en la cuenca cenozoica de As Pontes (La Coruña)es_ES
dc.titleFault analysis in the Cenozoic As Pontes Basin (La Coruña, NW Spain)eng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 15, (1993)