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http://hdl.handle.net/2445/105024
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DC Field | Value | Language |
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dc.contributor.author | Nebot Miralles, Marina | - |
dc.contributor.author | Guimerà i Rosso, Joan J. | - |
dc.date.accessioned | 2016-12-21T12:12:44Z | - |
dc.date.available | 2016-12-21T12:12:44Z | - |
dc.date.issued | 2016-07 | - |
dc.identifier.issn | 1576-5172 | - |
dc.identifier.uri | http://hdl.handle.net/2445/105024 | - |
dc.description.abstract | The Maestrat basin was one of the most subsident basins of the Iberian Rift system during the Late Jurassic- Early Cretaceous, generated by a normal fault system which divided it into sub-basins. The E-W-trending, N-verging Maestrat Basement Thrust developed during its Cenozoic inversion, traversing the entire basin, as a result of the inversion of the Mesozoic fault system within the basement. As this thrust reached the Mesozoic cover, it propagated across the Middle Muschelkalk detachment level, transporting the supra-salt cover, and the normal fault segments within it, about 11-13 km towards the North. The basement thrust is deduced to have a ramp-flat geometry, with a low dip ramp which reaches 8 km depth, rooted in the upper crust. The displacement of the basement in the hanging wall of this ramp generated a 40 km-wide uplifted area, in the N-S direction, bounded to the N by the Calders monocline, interpreted as a fault-bend-fold adapted to the ramp to flat transition in the basement thrust. It also indicates the transition from a thick-skinned style of deformation in the S, to a thin-skinned style to the N. The superficial shortening accumulated in the northern margin of the basin, containing the thinnest Mesozoic cover, developing the Portalrubio- Vandellòs fold-and-thrust belt. | - |
dc.format.extent | 4 p. | - |
dc.format.mimetype | application/pdf | - |
dc.language.iso | spa | - |
dc.publisher | Sociedad Geológica de España | - |
dc.relation.isformatof | Reproducció del document publicat a: | - |
dc.relation.ispartof | Geo-Temas, 2016, vol. 16, num. 2, p. 527-530 | - |
dc.rights | (c) Sociedad Geológica de España, 2016 | - |
dc.source | Articles publicats en revistes (Dinàmica de la Terra i l'Oceà) | - |
dc.subject.classification | Tectònica | - |
dc.subject.classification | Falles (Geologia) | - |
dc.subject.classification | Serralada Ibèrica | - |
dc.subject.other | Tectonics | - |
dc.subject.other | Faults (Geology) | - |
dc.subject.other | Iberian Mountains | - |
dc.title | Inversión cenozoica de la Cuenca mesozoica del Maestrat: evolución cinemática del cinturón de pliegues y cabalgamientos desarrollado en su margen norte (Cadena Ibérica oriental) | - |
dc.type | info:eu-repo/semantics/article | - |
dc.type | info:eu-repo/semantics/publishedVersion | - |
dc.identifier.idgrec | 666020 | - |
dc.date.updated | 2016-12-21T12:12:50Z | - |
dc.rights.accessRights | info:eu-repo/semantics/openAccess | - |
Appears in Collections: | Articles publicats en revistes (Dinàmica de la Terra i l'Oceà) |
Files in This Item:
File | Description | Size | Format | |
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666020.pdf | 899.59 kB | Adobe PDF | View/Open |
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