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Interplate versus intraplate strike-slip deformed belts: examples from SW Iberia

dc.contributor.authorRomão, J.
dc.contributor.authorRibeiro, Antonio
dc.contributor.authorPereira, E.
dc.contributor.authorRodrigues, J.
dc.contributor.authorA., Mateus
dc.contributor.authorNoronha, F.
dc.contributor.authorDias, R.
dc.date.accessioned2022-07-26T14:39:15Z
dc.date.available2022-07-26T14:39:15Z
dc.date.issued2010
dc.description.abstractA complete transition in tectonic style between pure thrust belts and pure strike-slip beltscan be envisaged, both in interplate and intraplate settings, by a combination of thrust and strike-slipcomponents of displacement. The accommodation of shortening components in strike-slip deforma-tion belts has been discussed recently on the basis of two alternative perspectives: (1) the “sub-horizon-tal attachment model”, where discrete strike-slip faulting of rigid blocks in the schiszosphere evolves tocontinuous movement in plastosphere through a bottom-up driving mechanism controlled by verticalcoupling across the lithosphere, and (2) the “accommodation model” that considers decoupling with-in a heterogeneous and anisotropic plastosphere. Two examples of variable shortening componentaccommodation in strike-slip deformation belts of the SW Iberia Variscides are reported and discussed.In the Tomar-Badajoz-Córdoba shear zone, an important shortening component is accommodated inflat-lying bends around the horizontal axis within a WNW-ESE flower-structure with sinistral strike-slip component; the geodynamic evolution points to an intraplate setting for this structure. In the N-S, Porto-Tomar-Ferreira do Alentejo, dextral shear zone, the shortening component is restricted torestraining bends around the vertical axis; the geodynamic evolution allows inferring a transformnature for this structure, thus indicating an interplate setting. For these examples, the “accommodationmodel” is preferred to the “sub-horizontal attachment model”pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.urihttp://hdl.handle.net/10451/53963
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherUniversidad de Oviedopt_PT
dc.relationPOCI/CTE-GIN/56445/2004pt_PT
dc.relation.publisherversionhttps://reunido.uniovi.es/index.php/TDG/article/view/180/178pt_PT
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/pt_PT
dc.subjectSW Iberia Variscidespt_PT
dc.subjectTectonicpt_PT
dc.titleInterplate versus intraplate strike-slip deformed belts: examples from SW Iberiapt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.endPage182pt_PT
oaire.citation.startPage176pt_PT
oaire.citation.titleTrabajos de Geologíapt_PT
oaire.citation.volume30pt_PT
person.familyNameRibeiro
person.familyNameNunes Mateus
person.givenNameAntonio
person.givenNameAntónio Manuel
person.identifierD-3727-2011
person.identifier.ciencia-id2A19-4EAC-B0F7
person.identifier.ciencia-id3012-5AFF-429F
person.identifier.orcid0000-0003-2623-1539
person.identifier.scopus-author-id6701374691
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublication3f9013fd-2dbe-477c-bb14-2bd3ba248dcf
relation.isAuthorOfPublication48cb5c2a-66a8-4389-a848-80813db2c9b0
relation.isAuthorOfPublication.latestForDiscovery3f9013fd-2dbe-477c-bb14-2bd3ba248dcf

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