Composite origin of an early Variscan transported suture: Ophiolitic units of the Morais Nappe Complex (north Portugal)
The two structural units that constitute the ophiolitic complex of the Morais allochthonous
complex display different geochemical features. Amphibolites from the lower unit are nearly …
complex display different geochemical features. Amphibolites from the lower unit are nearly …
[PDF][PDF] Património geomorfológico: conceptualização, avaliação e divulgação: aplicação ao Parque Natural de Montesinho
PJS Pereira - 2007 - repositorium.sdum.uminho.pt
Síntese Valor: valores científico e estético moderados, com controlo estrutural do relevo e
trajecto meandriforme do rio Maçãs. Potencialidades de uso: acessibilidade difícil e …
trajecto meandriforme do rio Maçãs. Potencialidades de uso: acessibilidade difícil e …
[HTML][HTML] A tectonic carpet of Variscan flysch at the base of a rootless accretionary prism in northwestern Iberia: U–Pb zircon age constrains from sediments and …
The allochthonous complexes of Galicia–Trás-os-Montes Zone (NW Iberia) are part of a
rootless tectonic stack which preserves part of a Variscan accretionary prism. They are …
rootless tectonic stack which preserves part of a Variscan accretionary prism. They are …
[PDF][PDF] The geological heritage on the Montesinho Natural Park (NE Portugal)–an interpretation strategy for an area with high geological complexity
DI Pereira, C Meireles, MIC Alves… - Natural and Cultural …, 2004 - natura.dct.uminho.pt
The geological complexity and the exotic character of several formations of the Montesinho
Natural Park (NE Portugal) print peculiar characteristics to the landscape. This part of the …
Natural Park (NE Portugal) print peculiar characteristics to the landscape. This part of the …
[PDF][PDF] Biodisponibilidad de metales en suelos y acumulación en plantas en el área de Trás-os-Montes (NE Portugal): influencia del material original
JD Lázaro, P Kidd, C Monterroso - Edafología, 2002 - academia.edu
Actualmente se reconoce que las técnicas de fitocorrección (uso de plantas para la
descontaminación de suelos) son alternativas prometedoras a las técnicas clásicas de …
descontaminación de suelos) son alternativas prometedoras a las técnicas clásicas de …
A tectonic carpet of Variscan flysch at the base of an unrooted accretion prism in NW Iberia: U-Pb zircon age constrains from sediments and volcanic olistoliths
The allochthonous complexes of Galicia–Trás-os-Montes Zone (NW Iberia) are part of the
tectonic stack that unrooted the Variscan accretionary prism. They are formed by individual …
tectonic stack that unrooted the Variscan accretionary prism. They are formed by individual …
Contribuição da palinologia para a caracterização paleoecológica e paleoclimática do Cenozóico a norte do Douro
MEP Poças - 2004 - repositorium.uminho.pt
O presente trabalho debruça-se sobre o estudo palínológíco de parte significativa dos
depósitos cenozóicos continentais do Norte de Portugal, no sentido da obtenção de …
depósitos cenozóicos continentais do Norte de Portugal, no sentido da obtenção de …
Património geomorfológico do sector oriental do Parque Natural de Montesinho (NE Portugal)
P Pereira, DI Pereira, MI Alves, C Meireles - 2002 - repositorium.uminho.pt
O Parque Natural de Montesinho (PNM) situa-se em Trás-os-Montes, no Nordeste de
Portugal, abrangendo a parte norte dos concelhos de Vinhais e Bragança e as serras da …
Portugal, abrangendo a parte norte dos concelhos de Vinhais e Bragança e as serras da …
[PDF][PDF] Silurian graptolite biostratigraphy of Portugal: an overview with notes on the Portuguese “Sardic” fauna
JM Piçarra - Proceedings of the 7th International Graptolite …, 2003 - researchgate.net
Silurian rocks are widely distributed within the Central Iberian and Ossa Morena Zones of
Portugal (Figure 1). They are known in two major tectono stratigraphic units of the Hesperian …
Portugal (Figure 1). They are known in two major tectono stratigraphic units of the Hesperian …
The geomorphological landscape of Trás-os-Montes and Alto Douro
The main geomorphological features of the eastern part of the Trás-os-Montes and Alto
Douro region are presented, namely the Iberian Meseta, the residual ridges, the Serra de …
Douro region are presented, namely the Iberian Meseta, the residual ridges, the Serra de …