Heinrich e Cécile Daniker-Haller - A música doméstica na vida de um casal de negociantes entre Zurique e o Rio de Janeiro na primeira metade do século XIX

O casal de suíços, Heinrich (1795–1866) e Cécile Däniker-Haller (1816–1887), com seus filhos, viveu no Rio de Janeiro entre 1828 e 1852. Comerciantes prósperos, cosmopolitas e melômanos, deixaram grande quantidade de informações sobre suas atividades de música em ambiente doméstico daquele período, mas também depois de terem voltado a se estabelecer na Suíça. O Genealogisches Archiv der Helene und Cécile Rübel Familienstiftung (FA HCR), na cidade de Zurique, documenta a história desta família. As informações registradas pelo casal estudado, principalmente em forma de cartas e diários, permitem-nos conhecer e analisar a prática musical em ambiente doméstico das famílias estrangeiras no Rio de Janeiro, e demonstrar quais eram os repertórios por eles utilizados. Entre as conclusões tiradas, inclui-se o fato de que o romantismo alemão teria feito sua entrada no ambiente musical brasileiro através dos salões musicais das famílias estrangeiras, exatamente como foi o caso em outras cidades do mundo não germânico. Nos documentos deixados pela família Däniker-Haller encontram-se os mais antigos testemunhos até hoje encontrados da execução de Lieder de Schubert em ambiente doméstico no Rio de Janeiro. Por outro lado, a prática da Hausmusik na cidade de Zurique vem descrita e comparada àquela carioca. A análise destes relatos também nos permite descrever a diferença que havia entre os eventos musicais em ambiente doméstico íntimo e informal, e os "salões musicais", onde diletantes se produziam em esfera semi-pública previamente preparados e ensaiados, e a marcante diferença no repertório destes dois tipos de eventos sociais.

An 40Ar/39Ar, Rb/Sr, and stable isotope study of micas in low-grade fold-and-thrust belt: An example from the Swiss Helvetic Alps

White micas in carbonate-rich tectonites and a few other rock types of large thrusts in the Swiss Helvetic fold-and-thrust belt have been analyzed by Ar-40/Ar-39 and Rb/Sr techniques to better constrain the timing of Alpine deformation for this region. Incremental Ar-40/Ar-39 heating experiments of 25 weakly metamorphosed (anchizone to low greenschist) samples yield plateau and staircase spectra. We interpret most of the staircase release spectra result from variable mixtures of syntectonic (neoformed) and detrital micas. The range in dates obtained within individual spectra depends primarily on the duration of mica nucleation and growth, and relative proportions of neoformed and detrital mica. Rb/Sr analyses of 12 samples yield dates of ca. 10-39 Ma (excluding one anomalously young sample). These dates are slightly younger than the Ar-40/Ar-39 total gas dates obtained for the same samples. The Rb/ Sr dates were calculated using initial Sr-87/Sr-86 ratios obtained from the carbonate-dominated host rocks, which are higher than normal Mesozoic carbonate values due to exchange with fluids of higher Sr-87/Sr-86 ratios (and lower O-18/O-16 ratios). Model dates calculated using Sr-87/Sr-86 values typical of Mesozoic marine carbonates more closely approximate the Ar-40/Ar-39 total gas dates for most of the samples. The similarities of Rb/Sr and Ar-40/Ar-39 total gas dates are consistent with limited amounts of detrital mica in the samples. The delta(18)O values range from 24-15%. (VSMOW) for 2-6 mum micas and 27-16parts per thousand for the carbonate host rocks. The carbonate values are significantly lower than their protolith values due to localized fluid-rock interaction and fluid flow along most thrust surfaces. Although most calcite-mica pairs are not in oxygen isotope equilibrium at temperatures of ca. 200-400 degreesC, their isotopic fractionations are indicative of either 1) partial exchange between the minerals and a common external fluid, or 2) growth or isotopic exchange of the mica with the carbonate after the carbonate had isotopically exchanged with an external fluid. The geological significance of these results is not easily or uniquely determined, and exemplifies the difficulties inherent in dating very fine-grained micas of highly deformed tectonites in low-grade metamorphic terranes. Two generalizations can be made regarding the dates obtained from the Helvetic thrusts: 1) samples from the two highest thrusts (Mt. Gond and Sublage) have all of their Ar-40/Ar-39 steps above 20 Ma, and 2) most samples from the deepest Helvetic thrusts have steps (often accounting for more than 80% of Ar-39 release) between 15 and 25 Ma. These dates are consistent with the order of thrusting in the foreland-imbricating system and increase proportions of neoformed to detrital mica in the more metamorphosed hinterland and deeply buried portions of the nappe pile. Individual thrusts accommodated the majority of their displacement during their initial incorporation into the foreland-imbricating system, and some thrusts remained active or were reactivated down to 15 Ma.

The newly defined "Greenstone Unit'' of the Aiguilles Rouges massif (western Alps): remnant of an Early Palaeozoic oceanic island-arc ?

In the southwestern part of the Aiguilles Rouges massif (pre-Alpine basement of the Helvetic realm, western Alps), a metavolcanic sequence, newly defined as the ``Greenstone Unit'',is exposed in two NS trending belts of several 100 metres in thickness. It consists of epidote amphibolites, partly epidote and/or calcic amphibole-bearing greenschists, and small amounts of alkali feldspar-bearing greenschists, which underwent low- to medium-grade metamorphism during Visean oblique collision. Metamorphic calcic amphiboles and epidotes show strong chemical zoning, whereas metamorphic plagioclase is exclusively albitic in composition (An 1-3). The SiO2 content of the subalkaline tholeiitic to calc-alkaline suite ranges continuously from 44 wt% to 73 wt%,but andesitic rocks predominate. The majority of samples have chemical compositions close to recent subduction-related lavas; some are even restricted to recent oceanic arcs (extremely low Ta and Nb contents, high La/Nb and Th/Ta ratios). But several basaltic to basalto-andesitic samples resemble continental tholeiites (low Th/Ta, La/Nb ratio). As it is very probable that both lava types are to some extent contemporaneous, it is proposed that the Greenstone Unit represents a former oceanic volcanic are which temporarily underwent extension during which emplacement of continental tholeiite-like rocks occurred. The cause of the extension remains ambiguous. Considering palaeotectonic significance and age of other metavolcanic units in the Aiguilles Rouges massif, the Greenstone Unit most likely formed in the Early Palaeozoic.

Geology of the Gander Group, Gander River Ultramafic Belt and Davidsville Group in the Jonathan's Pond - Weir's Pond Area, northeast Newfoundland /

The study area is situated in NE Newfoundland between Gander Lake and the north coast and on the boundary between the Gander and Botwood tectonostratigraphic zones (Williams et al., 1974). The area is underlain by three NE trending units; the Gander Group, the Gander River Ultramafic Belt (the GRUB) and the Davidsville Group. The easternmost Gander Group consists of a thick, psammitic unit composed predominantly of psammitic schist and a thinner, mixed unit of semipelitic and pelitic schist with minor psammite. The mixed unit may stratigraphically overlie the psammitic unit or be a lateral facies equivalent of the latter. No fossils have been recovered from the Gander Group. The GRUB is a terrain of mafic and ultramafic plutonic rocks with minor pillow lava and plagiogranite. It is interpreted to be a dismembered ophiolite in thrust contact with the Gander Group. The westernmost Davidsville Group consists of a basal conglomerate, believed deposited unconformably upon the GRUB from which it was derived, and an upper unit of greywacke and slate, mostly of turbidite origin, with minor limestone and calcareous sandstone. The limestone, which lies near the base of the unit, contains Upper Llanvirn to Lower Llandeilo fossils. The Gander and Davidsville Groups display distinctly different sedimentological , structural and metamorphic histories. The Gander Group consists of quartz-rich, relatively mature sediment. It has suffered three pre-Llanvirn deformations, of which the main deformation, Dp produced a major, NE-N-facing recumbent anticline in the southern part of the study area. Middle greenschist conditions existed from D^ to D- with growth of metamorphic minerals during each dynamic and static phase. In contrast, the mineralogically immature Davidsville Group sediment contains abundant mafic and ultramafic detritus which is absent from the Gander Group. The Davidsville Group displays the effects of a single penetrative deformation with localized D_ and D_ features, all of which can be shown to postdate D_ in the Gander Group. Rotation of the flat Gander S- into a subvertical orientation near the contact with the GRUB and the Davidsville Group is believed to be a Davidsville D^ feature. Regional metamorphism in the Davidsville Group is lower greenschist with a single growth phase, MS . These sedimentological, structural and metamorphic differences between the Gander and Davidsville Groups persist even where the GRUB is absent and the two units are in contact, indicating that the tectonic histories of the Gander and Davidsville Groups are distinctly different. Structural features in the GRUB, locally the result of multiple deformations, may be the result of Gander and/or Davidsville deformations. Metamorphism is in the greenschist facies. Geochemical analyses of the pillow lava suggest that these rocks were formed in a back-arc basin. Mafic intrusives in the Gander Group appear to be the result of magraatism separate from that producing the pillow lava. The Gander Group is interpreted to be a continental rise prism deposited on the eastern margin of the Late Precambrian-Lower Paleozoic lapetus Ocean. The GRUB, oceanic crust possibly formed in a marginal basin to the west, is believed to have been thrust eastward over the Gander Group, deforming the latter, during the pre-Llanvirnian, possibly Precambrian, Ganderian Orogeny. The Middle Ordovician and younger Davidsville Group was derived from, and deposited unconformably on, this deformed terrain. Deformation of the Davidsville Group occurred during the Middle Devonian Acadian Orogeny.

Denver and Rio Grande Railway schedule

Denver and Rio Grande Railway schedule, 1881.

Report of the Secretary of War, communicating; in compliance witha resolution of the Senate, a map showing the operations of the army of the United States in Texas and the adjacent Mexican Stateson the Rio Grande, accompanied by astronomical observations, and descriptive and military memoirs of the country.

UANL

Une urbanisation de corps et d'esprit : sécurité, civilisation et rendement dans une favela de Rio de Janeiro

Ce mémoire interroge l’histoire, l’articulation pratique et les effets de ce que l’on appelle actuellement au Brésil «l’urbanisation intégratrice», un type d’intervention étatique dans les favelas (bidonvilles) de Rio de Janeiro. Il s’agit d’une énième tentative de régler le «problème de la favela», consistant en l’urbanisation de son territoire (insertion d’infrastructure publique, consolidation du cadre bâti) et la légalisation de son statut et de ses pratiques (octroi de droits de propriété foncière et insertion de règlementation publique). Officiellement, c’est une manière de mettre fin à l’exclusion dont les populations faveladas sont victimes depuis l’apparition des favelas à Rio. L’analyse est faite à partir de l’étude du PAC-Favelas, un programme du gouvernement fédéral lancé en 2008, et son application dans la favela Rocinha. Il est proposé de considérer l’urbanisation intégratrice en tant que dispositif sécuritaire ou biopolitique, c’est-à-dire en tant qu’appareil de gouvernement de la population locale. À travers le projet, on planifie de formaliser les conduites, d’accroître la circulation des ressources, de transformer les perceptions des résidents, de contenir les excès et les risques associés à la favela et de tendre vers la prise en charge entièrement planifiée – en un mot, d’assurer le passage vers l’intervention permanente. Concrètement, cela revient pour l’État à procéder à une sélection, par des moyens légitimés ou indirects (le plan, la loi, le marché), des individus et des pratiques désormais admissibles sur le territoire. L’espace se raréfie, le contrôle augmente et les prix montent : ne peut demeurer que celui qui a déjà atteint un certain niveau de stabilité, reléguant les plus précaires à devoir progressivement quitter le territoire. Urbaniser la Rocinha, c’est un peu forcer son embourgeoisement en la rendant enfin sécurisée, civilisée et rentable.

La culture comme ressource : des groupes musicaux populaires au sein du processus de réaménagement urbain à Rio de Janeiro

Ce projet de maîtrise porte sur l’interaction entre les acteurs locaux liés à la musique populaire et l’administration publique dans le cadre du projet public-privé de réaménagement du port de Rio de Janeiro intitulé Porto Maravilha. Le travail de recherche s’est axé sur l’idée que cette interaction serait essentiellement fondée sur la façon dont la “culture” est comprise et utilisée comme ressource capable d’ajouter de la valeur à l’espace urbain, différencier les groupes entre eux et apporter une sustentation au processus d’autonomisation et de légitimation des acteurs. De nouveaux paradigmes urbanistiques, tel celui de “ville créative” (Landry, 2005), proposent d’intégrer la culture locale dans l’élaboration et l’exécution des projets avec la participation d’artistes qui sont perçus comme une source de créativité fondamentale pour rendre la ville plus compétitive dans un monde devenu de plus en plus urbain. Dans cette veine, le projet Porto Maravilha s’inspire franchement des cas de succès de rénovation urbaine créative, stimulant la culture locale et idéalisant le port de Rio comme une “nouvelle carte postale du Brésil”. En partant de la constatation que les acteurs sociaux locaux identifient le potentiel de leurs activités culturelles comme une ressource importante dans ce contexte, nous analysons tout autant les stratégies et les discours élaborés que les ressources dont ils disposent afin d’affirmer leur agentivité. Au-delà de l’action intentionnelle, nous effectuons également des analyses de leurs pratiques culturelles au quotidien en recherchant les éléments qui les constituent. Nous questionnons, par ailleurs, la manière avec laquelle les administrateurs du projet comprennent ces activités musicales et comment ils gèrent les demandes sociales et les contributions créatives de ces groupes.