Publication
Interplate versus intraplate strike-slip deformed belts: examples from SW Iberia
| dc.contributor.author | Romão, J. | |
| dc.contributor.author | Ribeiro, Antonio | |
| dc.contributor.author | Pereira, E. | |
| dc.contributor.author | Rodrigues, J. | |
| dc.contributor.author | A., Mateus | |
| dc.contributor.author | Noronha, F. | |
| dc.contributor.author | Dias, R. | |
| dc.date.accessioned | 2022-07-26T14:39:15Z | |
| dc.date.available | 2022-07-26T14:39:15Z | |
| dc.date.issued | 2010 | |
| dc.description.abstract | A 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.version | info:eu-repo/semantics/publishedVersion | pt_PT |
| dc.identifier.uri | http://hdl.handle.net/10451/53963 | |
| dc.language.iso | eng | pt_PT |
| dc.peerreviewed | yes | pt_PT |
| dc.publisher | Universidad de Oviedo | pt_PT |
| dc.relation | POCI/CTE-GIN/56445/2004 | pt_PT |
| dc.relation.publisherversion | https://reunido.uniovi.es/index.php/TDG/article/view/180/178 | pt_PT |
| dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/4.0/ | pt_PT |
| dc.subject | SW Iberia Variscides | pt_PT |
| dc.subject | Tectonic | pt_PT |
| dc.title | Interplate versus intraplate strike-slip deformed belts: examples from SW Iberia | pt_PT |
| dc.type | journal article | |
| dspace.entity.type | Publication | |
| oaire.citation.endPage | 182 | pt_PT |
| oaire.citation.startPage | 176 | pt_PT |
| oaire.citation.title | Trabajos de Geología | pt_PT |
| oaire.citation.volume | 30 | pt_PT |
| person.familyName | Ribeiro | |
| person.familyName | Nunes Mateus | |
| person.givenName | Antonio | |
| person.givenName | António Manuel | |
| person.identifier | D-3727-2011 | |
| person.identifier.ciencia-id | 2A19-4EAC-B0F7 | |
| person.identifier.ciencia-id | 3012-5AFF-429F | |
| person.identifier.orcid | 0000-0003-2623-1539 | |
| person.identifier.scopus-author-id | 6701374691 | |
| rcaap.rights | openAccess | pt_PT |
| rcaap.type | article | pt_PT |
| relation.isAuthorOfPublication | 3f9013fd-2dbe-477c-bb14-2bd3ba248dcf | |
| relation.isAuthorOfPublication | 48cb5c2a-66a8-4389-a848-80813db2c9b0 | |
| relation.isAuthorOfPublication.latestForDiscovery | 3f9013fd-2dbe-477c-bb14-2bd3ba248dcf |
