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.

Currículo no ensino fundamental de nove anos: uma análise das possíveis mudanças curriculares nas séries iniciais da rede estadual de ensino de Santa Catarina - Brasil

Diante da medida política, de cunho educativo, de ampliação do Ensino Fundamental brasileiro de oito para nove anos de escolaridade obrigatória, esta investigação propôs-se analisar os reflexos desta deliberação na proposta curricular oficialmente prescrita. A questão da qual se ocupou este estudo, é portanto: Quais as mudanças de natureza curricular, nas Séries Iniciais da Rede Estadual de Ensino de Santa Catarina, decorrentes das alterações estabelecidas pela Lei n. 11.274? Este estudo caracteriza-se por uma pesquisa documental, de abordagem histórica e qualitativa, cujo método de investigação é a técnica de análise de conteúdo. A análise dos Documentos Preliminares de Seleção e Organização Curricular para as Séries Iniciais do Ensino Fundamental de Nove Anos, permitiu-nos inferir que não houve mudanças significativas na organização curricular quando comparada com a Proposta Curricular de Santa Catarina elaborada anteriormente; ### ABSTRACT: NINE YEARS ELEMENTARY EDUCATION CURRICULUM: An analysis of the possible curriculum changes in the Elementary School first grades in Santa Catarina State – Brazil This investigation purposes to examine the policy measure, in a educative way, of the brazilian Elementary Education extension, from eight to nine required years, as also this decision´s consequences in the officially prescribed curriculum proposal. The question which this study has engaged is, therefor: what are the results of the first grade of elementary school curricular changes in Santa Catarina, according with the law n. 11.274? This study describes a documentary research, with a historical and qualitative approach, which investigation method is a content analysis technique. The analysis of the Curricular Preliminary Selection and Organization Documents to the Nine Years Elementary Education allowed us to conclude that no meaning changes have occurred in the curricular organizaton, when compared with the previous proposal.