Encontrados 5 documentos, a visualizar página 1 de 1
Chronic stress disrupts neural coherence between cortico-limbic structures
Dias, Nuno S.; Oliveira, João Filipe; Correia, Mariana; Gama-Pereira, Filipa; Sardinha, Vanessa Morais; Lima, Ana; Oliveira, Ana FilipaChronic stress impairs cognitive function, namely on tasks that rely on the integrity of cortico-limbic networks. To unravel the functional impact of progressive stress in cortico-limbic networks we measured neural activity and spectral coherences between the ventral hippocampus (vHIP) and the medial prefrontal cortex (mPFC) in rats subjected to short term stress (STS) and chronic unpredictable stress (CUS). CU...
Avaliação museológica : estudo de caso : avaliação de exposição permanente do M...
Guapo, Amanda Lúcia Gama Pereira DiasDissertação de mestrado em Museologia e Património Cultural, apresentada à Faculdade de Letras da Universidade de Coimbra
Avaliação museológica : estudo de caso : avaliação de exposição permanente do M...
Guapo, Amanda Lúcia Gama Pereira DiasDissertação de mestrado em Museologia e Património Cultural, apresentada à Faculdade de Letras da Universidade de Coimbra
Shadowing effects on beach morphodynamics during storm events on Tróia-Sines em...
Jacob, José; Gama, Pereira; Salgado, Rui; Liu, James; Silva, Ana MariaThe prediction of storm effects on coastline is essential to coastal management and represents a critical issue for the scientific community discussion. In this paper we used SWAN and Méso-NH models to simulate the wave pattern along a ten’s kilometre-scale sandy coastline (TSEC, Tróia-Sines Embayed Coast). The obtained results indicate a shelter effect of the Espichel Cape in the northern half of the TSEC for ...
Tectonostratigraphy of Middle and Upper Palaeozoic black shales from the Porto-...
Chaminé, H. I.; Gama Pereira, L. C.; Fonseca, P. E.; Fernandes, J. P.; Rocha, F. T.; Flores, D.; Pinto de Jesus, A.; Gomes, C.; Soares de Andrade, A. AAbstract Middle/late Devonian and early Carboniferous metasedimentary sequences in the northernmost region (Porto-Espinho-Tomar) of the Ossa-Morena Zone (Portuguese Iberian Variscan Massif) contain black shales of very low to low-grade metamorphism. These metasedimentary rocks form a discrete NNW-SSE structure within a major shear zone (Porto-Tomar-Ferreira do Alentejo) and remain subparallel to the observed re...
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