U-Pb geochronology and Nd isotope contributions to the interpretation of a peculiar ring massif: the Santa Eulália plutonic complex (SW Iberia, Portugal)

The Santa Eulalia plutonic complex (SEPC) is a late-Variscan granitic body placed in the Ossa-Morena Zone. The host rocks of the complex belong to metamorphic formations from Proterozoic to Lower Paleozoic. The SEPC is a ring massif (ca. 400 km2 area) composed by two main granitic facies with different colours and textures. From the rim to the core, there is (i) a peripheral pink medium- to coarse-grained granite (G0 group) involving large elongated masses of mafic and intermediate rocks, from gabbros to granodiorites (M group), and (ii) a central gray medium-grained granite (G1 group). The mafic to intermediate rocks (M group) are metaluminous and show wide compositions: 3.34–13.51 wt% MgO; 0.70–7.20 ppm Th; 0.84–1.06 (Eu/Eu*)N (Eu* calculated between Sm and Tb); 0.23–0.97 (Nb/Nb*)N (Nb* calculated between Th and La). Although involving the M-type bodies and forming the outer ring, the G0 granites are the most differentiated magmatic rocks of the SEPC, with a transitional character between metaluminous and peraluminous: 0.00–0.62 wt% MgO; 15.00–56.00 ppm Th; and 0.19–0.42 (Eu/Eu*)N ; 0.08–0.19 (Nb/Nb*)N [1][2]. The G1 group is composed by monzonitic granites with a dominant peraluminous character and represents the most homogeneous compositional group of the SEPC: 0.65–1.02 wt% MgO; 13.00–16.95 ppm Th; 0.57–0.70 (Eu/Eu*)N ; 0.14–0.16 (Nb/Nb*)N . According to the SiO2 vs. (Na2O+K2O–CaO) relationships, the M and G1 groups predominantly fall in the calc-alkaline field, while the G0 group is essencially alkali-calcic; on the basis of the SiO2 vs. FeOt/(FeOt+MgO) correlation, SEPC should be considered as a magnesian plutonic association [3]. New geochronological data (U-Pb on zircons) slightly correct the age of the SEPC, previously obtained by other methods (290 Ma, [4]). They provide ages of 306  2 Ma for the M group, 305  6 Ma for the G1 group, and 301  4 Ma for the G0 group, which confirm the late-Variscan character of the SEPC, indicating however a faintly older emplacement, during the Upper Carboniferous. Recent whole-rock isotopic data show that the Rb-Sr system suffered significant post-magmatic disturbance, but reveal a consistent set of Sm-Nd results valuable in the approach to the magmatic sources of this massif: M group (2.9 < Ndi < +1.8); G1 group (5.8 < Ndi < 4.6); G0 group (2.2 < Ndi < 0.8). These geochemical data suggest a petrogenetic model for the SEPC explained by a magmatic event developed in two stages. Initially, magmas derived from long-term depleted mantle sources (Ndi < +1.8 in M group) were extracted to the crust promoting its partial melting and extensive mixing and/or AFC magmatic evolution, thereby generating the G1 granites (Ndi < 4.6). Subsequently, a later extraction of similar primary magmas in the same place or nearby, could have caused partial melting of some intermediate facies (e.g. diorites) of the M group, followed by magmatic differentiation processes, mainly fractional crystallization, able to produce residual liquids compositionally close to the G0 granites (Ndi < 0.8). The kinetic energy associated with the structurally controlled (cauldron subsidence type?) motion of the G0 liquids to the periphery, would have been strong enough to drag up M group blocks as those occurring inside the G0 granitic ring.

Pontes invisíveis. Estratégias de actuação de redes sociais no combate à pobreza e exclusão social: Um estudo de caso com redes sociais portuguesas

As Redes Sociais, enquanto estrutura social, são um sistema aberto, altamente dinâmico e susceptível de inovação (Castells, 2000) constituindo-se como um importante recurso para combater a pobreza e a exclusão social, através de uma acção concertada e coerente. No presente estudo, apresentam-se os resultados de um estudo qualitativo cujo objectivo foi o de conhecer os benefícios da actuação em rede como estratégia de combate à pobreza e exclusão social. Realizou-se uma entrevista semi-estruturada a 13 colaboradores de organizações, não-lucrativas, que operam em rede. As respostas foram analisadas a partir da metodologia qualitativa Consesual Qualitative Research (Clara Hill, 1997). Os resultados obtidos permitiram obter como principal atributo estratégico, da actuação em rede, a orientação para o processo, enquanto medida adaptável e geradora de resultados. As conclusões obtidas são discutidas quanto ao seu contributo para incentivar as políticas sociais que considerem o reconhecimento e activação da solidariedade social local. / ABSTRACT: Social Networks, as a social structure, are an open system, highly dynamic and capable of innovation (Castells, 2000) constituting itself as an important resource to combat Poverty and Social Exclusion, through a concerted and coherent action. ln this study, we present the results of a qualitative investigation whose aim was to know the benefits of building social networks of support in fighting against poverty and social exclusion. There were performed semi-structured interviews with 13 employees of non­profit organizations, operating in network. The responses were analyzed based on Consensual Qualitative Research (Clara Hill, 1997). The results have enabled the orientation to process as the main strategic attribute of the implementation Strategies of Social Network as an adaptive measure and as capable of generating results. The main conclusions are discussed in terms of its contribution to promote social policies that consider the recognition and activation of local charities.