Please use this identifier to cite or link to this item:
https://hdl.handle.net/10316/15201
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Cunha, P. Proença | - |
dc.contributor.author | Pereira, D. Insua | - |
dc.date.accessioned | 2011-04-27T22:56:43Z | - |
dc.date.available | 2011-04-27T22:56:43Z | - |
dc.date.issued | 2000 | en_US |
dc.identifier.citation | Cunha, Pedro P.; Pereira, D.I.Evolução cenozóica da área de Longroiva-Vilariça (NE Portugal), Ciências da Terra (UNL), 14, 89-198, 2000. | en_US |
dc.identifier.issn | 0254-055X | - |
dc.identifier.uri | https://hdl.handle.net/10316/15201 | - |
dc.description.abstract | In the Longroiva-Vilariça area, the identification of Cenozoic lithostratigraphic units, the sedimentology and the characterization of its geometric relations with tectonic structures allowed the interpretation of the palaeogeographic main stages: 1) the greenwhitish Vilariça Arkoses (Middle Eocene to Oligocene ?) represent proximal sediments of a very low gradient drainage towards the eastern Spanish Tertiary Duero Basin; 2)Quintãs Formation (late Miocene ?) are brown-reddish coloured piedmont alluvial deposits, correlative of important vertical displacement (western tectonic block relative uplift) along the NNE-SSW indent-linked strike-slip Bragança-Vilariça-Longroiva fault zone, interpreted as a reactivated deep hercynian fracture, with left-lateral movement; 3) the red Sampaio Formation (Gelasian-early Pleistocene ?)was interpreted as downhill conglomeratic deposits related with important overtrusting along this fault zone (the definition of the present-day narrow graben configuration) and correlative of the atlantic hydrographic incision stage beginning; 4) conglomeratic terraces (middle and late Pleistocene ?); 5) alluvial plains and colluvial deposits (Holocene). | - |
dc.language.iso | por | - |
dc.publisher | Universidade Nova de Lisboa | - |
dc.rights | openAccess | - |
dc.subject | Litostratigrafia | - |
dc.subject | Ambientes aluviais | - |
dc.subject | Depósitos siliciclásticos | - |
dc.subject | Neotectónica | - |
dc.subject | Descontinuidades sedimentares | - |
dc.subject | Cenozóico | - |
dc.title | Evolução cenozóica da área de Longroiva-Vilariça (NE Portugal) | en_US |
dc.type | article | - |
degois.publication.firstPage | 89 | - |
degois.publication.lastPage | 98 | - |
degois.publication.issue | Ciências da Terra (UNL) | - |
degois.publication.issue | 14 | - |
dc.date.updated | 2011-04-27T22:56:44Z | - |
uc.controloAutoridade | Sim | - |
item.fulltext | Com Texto completo | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.grantfulltext | open | - |
item.languageiso639-1 | pt | - |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
crisitem.author.researchunit | MARE - Marine and Environmental Sciences Centre | - |
crisitem.author.orcid | 0000-0002-9956-4652 | - |
Appears in Collections: | I&D CGUC - Artigos em Revistas Nacionais FCTUC Ciências da Terra - Artigos em Revistas Nacionais |
Files in This Item:
File | Description | Size | Format | |
---|---|---|---|---|
Evolução cenozóica da área de Longroiva-Vilariça.pdf | 2.45 MB | Adobe PDF | View/Open |
Google ScholarTM
Check
Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.