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.

A arquitectura do mosteiro cartusiano de Santa Maria Scala Coeli: do processo de entrada

A importância da encenação de uma transição entre o mundo secular e a vida em clausura, no contexto da arquitectura cartusiana, é amplamente demonstrada através dos percursos de entrada dos conjuntos mais relevantes, bem como em muitos daqueles representados nas gravuras presentes no livro Maisons de l’Ordre des Chartreux – Vues et Notices, uma obra do início do século XX que inclui gravuras da quase totalidade dos 282 mosteiros cartusianos distribuídos por quase toda a Europa. Na maioria das cartuxas podem observarse transições indirectas e prolongadas, capazes de tardar o passo e dar significado à passagem para a clausura – características espaciais que São Bruno, fundador da casa cartusiana, considerava primordiais para a implantação do seu eremitério. A partir de uma cuidada análise dessa transição, nas cartuxas em geral, e da sua evolução morfológica, na cartuxa de Évora em particular – estimulada pela descoberta de dados aqui analisados e interpretados pela primeira vez – apresenta-se, em continuidade com a sua história e tendo como premissa a consolidação do processo de entrada, uma proposta de redefinição da estrutura monacal de Santa Maria Scala Coeli. Esta estrutura originária do século XVI encontra-se incompleta e degradada, em particular na ala sul onde se encontra o seu principal acesso, sendo fundamental o completamento desta área para o cabal reconhecimento da unidade do conjunto e da intenção na qual se traduz a sua génese. De resto, a estratégia de investigação e de projecto descrita nesta dissertação pode ser encarada como um processo plausível de ser utilizado no caso de futuras intervenções noutras estruturas cartusianas, contribuindo assim para a recuperação e preservação do conceito fundador da identidade da arquitectura cartusiana que, no decorrer da expansão da ordem, se foi perdendo; The Architecture of the Carthusian Monastery of Santa Maria Scala Coeli: About the process of entrance. ABSTRACT: The importance of staging a transition between the secular world and life cloistered in the context of Carthusian architecture is amply demonstrated through the input paths of the most important collections, as well as many of those represented in the pictures in the book Maisons de l’Ordre des Chartreux – Vues et Notices, one of the early twentieth century work that includes prints of almost all of the 282 Carthusians monasteries spread across almost all of Europe. In most of Carthusian the transitions that can be observed are indirect and long, able to delay the step and give meaning to the passage to the life cloistered - spatial characteristics that St. Bruno, founder of the Carthusian Order, considered essential for the implementation of his hermitage. From a careful analysis of this transition, looking through the Carthusian in general, and its morphological evolution, in the Charterhouse of Évora in particular, encouraged by the data discovery here analyzed and interpreted for the first time - it is presented in continuity with its history and having premised on the consolidation of the entry process, a proposal for a redefinition of the monastic structure of Santa Maria Scala Coeli. This original structure of the sixteenth century is incomplete and degraded, particularly in the south wing where it is the main access, and where is fundamental the completion of this area to the full recognition of the unity of the whole and to understand the intent in which translates its genesis. Moreover, the research strategy and project described in this paper can be seen as a plausible case to be used in case of future interventions in other cartusianas structures, thus contributing to the recovery and preservation of the founder of the identity concept of the Carthusian architecture that, during the expansion of the order, was missing.