Tekstiilitaiteilija Dora Jung 15/1 1972

Kirje 15.1.1972

As interfaces entre imagem corporal e a representação simbolica de Carl Gustav Jung

Universidade Estadual de Campinas . Faculdade de Educação Física

Freud e Johnson-Laird: Modelos Mentais no «Caso Dora»

Trabalho sobre a relação entre a teoria dos modelos mentais de Johnson-Laird e o conceito de transferência em Freud.

Las relaciones de las teorías de Jung y el trabajo de Grotowski con sus actores

La finalidad del trabajo es demostrar que los objetivos que Grotowski pretendió en su trabajo con los actores en su primera época, ligada al teatro laboratorium, pueden ser contemplados desde el mapa conceptual de la psicología profunda o analítica creada por C.G. Jung. Este acercamiento, permite reimaginar este “proceso de autopenetración” que el creador polaco buscaba con sus actores desde esta visión psicológica concreta. Cabe afirmar, por tanto, que este trabajo actoral iba más allá de la dimensión escénica y era un método “terapéutico” de desarrollo de la personalidad del individuo-actor en su camino de transformación para llegar a ser lo que Grotowski denominó “actor santo”.

Trabalhando com a história de vida: percalços de uma pesquisa(dora?)

Trata-se de um estudo de natureza qualitativa, cuja autora relata a sua experiência na realização da tese de Doutorado pelo método de História de Vida. Descreve a abordagem metodológica, explicitando a técnica para a coleta e a análise dos relatos bem como as eventuais dificuldades que possam surgir durante a realização da pesquisa. Argumenta que esse método possibilita a aproximação entre o pesquisador e os sujeitos. Destaca a necessidade de se incluir a dimensão subjetiva do cuidado na prestação de assistência à clientela.

U-Pb zircon dating of granitoids from the Dora-Maira massif (western Italian Alps)

Among the large number of granitic intrusions within the Dora-Maira massif, several main types can be distinguished. In this study we report field, petrographic and geochemical investigations as well as zircon typology and conventional U-Pb zircon dating of plutons representing these types. The main results are as follows: the Punta Muret augengneiss is a polymetamorphosed peraluminous granite of anatectic origin. It is 457 +/- 2 Ma old and represents one of the numerous Caledonian orthogneisses of the Alpine basement. All other dated granites are of Late Variscan age. The Cavour leucogranite is an evolved granite of probably calc-alkaline affiliation, dated at 304 +/- 2 Ma. The dioritic and granodioritic facies of the Malanaggio diorite (auct.) are typical calc-alkaline rocks, whose respective age of 290 +/- 2 and 288 +/- 2 Ma overlap within errors. The Sangone and Freidour granite types have very similar alkali-calcic characteristics; their ages are poorly constrained between 267-279 and 268-283 Ma, respectively. The new data for the Dora-Maira granites are in keeping with models of the overall evolution of the Late- to Post-Variscan magmatism in the Alpine area in terms of age distribution and progressive geochemical evolution towards alkaline melts. In a first approximation, granitic rocks across the Variscan belt seem to be increasingly younger towards the internal (southern) parts of the orogen. A Carboniferous, distensive Basin and Range situation is thought to be responsible for the magmatic activity. This tectonic context is comparable to the back-are opening of an active continental margin. The observed southward migration of the magmatism could be linked to the roll-back of the subducting Paleotethyan oceanic plate along the Variscan cordillera.

Biblioteca universitaria, CRAI y alfabetización informacional (María Pinto, Dora Sales y Pilar Osorio)

DURANTE LA CELEBRACIÓN EN LA UNIVERSITAT DE BARCELONA (marzo de 2008) de la Conferencia de primavera de la EUA (European University Association), se ha definido la estrategia a seguir para consolidar los retos del EEES (Espacio Europeo de Educación Superior) y del EEI (Espacio Europeo de Investigación).

Geochemistry and 40Ar/39Ar geochronology of pseudotachylyte associated with UHP whiteschists from the Dora Maira massif, Italy

In situ UV-Iaser ablation Ar-40/(39) Ar geochronological and geochemical data, together with rock and mineral compositional data, have been determined from pseudotachylyte and surrounding mylonitic gneiss associated with the UHP whiteschists of the Dora Maira Massif, Italy. Several generations of fresh pseudotachylyte occur as irregular veins up to a few cur thick both parallel and at high angles to the foliation. Whole rock XRF data collected from representative lithologies of mylonitic gneiss are uniformly consistent with a mildly alkalic granitic protolith. Minimal compositional variation is observed between the pseudotachylyte and its surrounding mylonitic gneiss. The pseudotachylyte contains newly crystallized grains of biotite and K-feldspar in a matrix of glass with partially fused grains of quartz, zircon, apatite, and titanite. Electron microprobe analyses of the glass show significant compositional variation that is probably strongly influenced by micrometer-scale changes in mineralogy. UV-Iaser ablation ICP-MS traverses across the mylonitic gneiss-pseudotachylyte contact are consistent with cataclastic communition of REE carriers such as epidote, monazite, allanite, zircon, and apatite before melting as an efficient mechanism of REE homogenization in the pseudotachylyte. The 40Ar/39Ar data from one band of pseudotachylyte indicate formation at 20.1 +/- 0.5 Ma, when the mylonitic gneisses were already in a near surface position. The variable effects of top-to-the-west shear deformation within outcrops of the coesite-bearing unit are reflected in localized zones of protomylonite, cataclasite, ultracataclasite, and pseudotachylyte. Preservation of several generations of pseudotachylyte suggests that seismic events may have played a significant role in triggering late unroofing of the UHP rocks. It is speculated that deeper crustal seismic events potentially played a role in the unroofing of the UHP rocks at earlier stages in their exhumation history. (c) 2005 Elsevier B.V. All rights reserved.