Reflexiones sobre ideología e interpelación en las elecciones presidenciales de 2015 en Argentina

En este trabajo abordamos del papel de la ideología y distintas formas de interpelación en las elecciones presidenciales de Argentina en 2015.Partimos de dos imputaciones cruzadas: la que surge del kirchnerismo, enfatizando el rol de los medios de comunicación masivos sobre los sectores medios y populares, y la respuesta progresista que insiste en una serie de motivos materiales de insatisfacción de estos sectores, a los que el kirchnerismo, afectado por una "miopía política", no atendió durante su gobierno y a los que desconoció en su discurso de campaña electoral, dejándolos librados a la interpelación por una forma de "individualismo miope". Insistimos en que estas atribuciones cruzadas de ideologismo constituyen un campo ideológico por sí mismo, cuyo presupuesto común es el individualismo. A partir de allí intentamos comprender las condiciones histórico-políticas en la Argentina del siglo XX que hacen del individualismo una evidencia ideológica fundante en la Argentina del siglo XXI

Reflexiones sobre ideología e interpelación en las elecciones presidenciales de 2015 en Argentina

En este trabajo abordamos del papel de la ideología y distintas formas de interpelación en las elecciones presidenciales de Argentina en 2015.Partimos de dos imputaciones cruzadas: la que surge del kirchnerismo, enfatizando el rol de los medios de comunicación masivos sobre los sectores medios y populares, y la respuesta progresista que insiste en una serie de motivos materiales de insatisfacción de estos sectores, a los que el kirchnerismo, afectado por una "miopía política", no atendió durante su gobierno y a los que desconoció en su discurso de campaña electoral, dejándolos librados a la interpelación por una forma de "individualismo miope". Insistimos en que estas atribuciones cruzadas de ideologismo constituyen un campo ideológico por sí mismo, cuyo presupuesto común es el individualismo. A partir de allí intentamos comprender las condiciones histórico-políticas en la Argentina del siglo XX que hacen del individualismo una evidencia ideológica fundante en la Argentina del siglo XXI

Explicacion de la Bula de la Santa Cruzada ... /

Encabezamiento tomado de Palau.

Epaeneticon historico-poeticum ad heroicos Viennae a numerosissimo Turcarum exercitu obsessae defensores ... /

Mode of access: Internet.

Compendio de las Tres Gracias de la Santa Cruzada, subsidio, y escusado, que su santidad concede a ... Felipe III ... para gastos de la guerra contra infieles, y la practica dellas ... /

Mode of access: Internet.

Niketou Akominatou Choniatou Historia = Nicetae Acominati Choniatae, magni logothetae secretorum, inspectoris et judicis veli, praefecti sacri cubiculi, Historia /

Incluye: Chronologia Nicetae, quae annorum ab eo descriptorum, & rerum sub imperatoribus gestarum seriem paucis indicat ; Glossarium, in quo vocabula graecobarbara explicantur ; Variae lectiones et annotationes in Nicetae Choniatae historiam / per Hieronymum Wolfium ; Gnomologia, id est, index sententiarum, quae ex Nicetae Choniatae historia collectae, & ordine alphabeti digestae sunt ; Axiomatum, et insignium quarundam sententiarum, quae in notis ad Nicetae historiam occurrunt, index.

Reflexiones sobre ideología e interpelación en las elecciones presidenciales de 2015 en Argentina

En este trabajo abordamos del papel de la ideología y distintas formas de interpelación en las elecciones presidenciales de Argentina en 2015.Partimos de dos imputaciones cruzadas: la que surge del kirchnerismo, enfatizando el rol de los medios de comunicación masivos sobre los sectores medios y populares, y la respuesta progresista que insiste en una serie de motivos materiales de insatisfacción de estos sectores, a los que el kirchnerismo, afectado por una "miopía política", no atendió durante su gobierno y a los que desconoció en su discurso de campaña electoral, dejándolos librados a la interpelación por una forma de "individualismo miope". Insistimos en que estas atribuciones cruzadas de ideologismo constituyen un campo ideológico por sí mismo, cuyo presupuesto común es el individualismo. A partir de allí intentamos comprender las condiciones histórico-políticas en la Argentina del siglo XX que hacen del individualismo una evidencia ideológica fundante en la Argentina del siglo XXI

Análise estratigráfica de subsuperfície do Devoniano Inferior da Bacia do Rio do Peixe, Nordeste do Brasil

Subsurface stratigraphic analysis of Devonian strata from the Rio do Peixe Basin, newly recognized by palynological studies, has resulted in the identification of two new lithostratigraphic units assembled in the Santa Helena Group. The Pilões Formation, the lower unit, is composed mainly of dark mudstones and medium-tovery fine-grained sandstones, with minor conglomerates and breccias. The Triunfo Formation, the upper unit, comprises whitish grey, kaolinitic, coarse-grained to conglomeratic, cross stratified sandstones and conglomerates, with interbedded mudstones and fine-grained sandstones. These units were characterized using cores, sidewall and cuttings samples, conventional logs and image log, from three wells drilled by PETROBRAS, and 3D seismic data. The Pilões Formation is interpreted as prodeltaic facies, with lesser associated subaqueous talus, debrite and sandy turbidite lobe facies, distal part of fandelta and braided fluviodeltaic facies of Triunfo Formation. The Santa Helena Group corresponds to the Lower Devonian tectono-sequence deposited in a NW-SE-trending graben during a transgressiveregressive cycle. With 343 meters of thickness (isochore) in well 1-PIL-1-PB (Pilões 1), this sequence has a non-conformity at the lower boundary and its upper boundary is an unconformity with the Lower Cretaceous tectono-sequence (Rio do Peixe Group), that represents a hiatus of about 265 million years. Ignimbrites and coignimbrite breccias (Poço da Jurema volcanic breccia), related to an unknown pyroclastic volcanic event, were recognized at the northern margin of the Sousa halfgraben. Evidence from well data suggests that this event is coeval with the Devonian graben filling. The present study indicates a polyhistorical tectono-volcanosedimentary evolution of the basin. This lithostratigraphic update brings new perspectives for geological research in the Rio do Peixe Basin, as well as in other inland basins of the Northeastern of Brazil. The results of the research also contribute to the kwnoledge of the Borborema Province and western Gondwana paleogeography during the Early Devonian.

Estudo da estrutura subsuperficial da província Borborema com correlação de ruído sísmico

Ambient seismic noise has traditionally been considered as an unwanted perturbation in seismic data acquisition that "contaminates" the clean recording of earthquakes. Over the last decade, however, it has been demonstrated that consistent information about the subsurface structure can be extracted from cross-correlation of ambient seismic noise. In this context, the rules are reversed: the ambient seismic noise becomes the desired seismic signal, while earthquakes become the unwanted perturbation that needs to be removed. At periods lower than 30 s, the spectrum of ambient seismic noise is dominated by microseism, which originates from distant atmospheric perturbations over the oceans. The microsseism is the most continuous seismic signal and can be classified as primary – when observed in the range 10-20 s – and secondary – when observed in the range 5-10 s. The Green‘s function of the propagating medium between two receivers (seismic stations) can be reconstructed by cross-correlating seismic noise simultaneously recorded at the receivers. The reconstruction of the Green‘s function is generally proportional to the surface-wave portion of the seismic wavefield, as microsseismic energy travels mostly as surface-waves. In this work, 194 Green‘s functions obtained from stacking of one month of daily cross-correlations of ambient seismic noise recorded in the vertical component of several pairs of broadband seismic stations in Northeast Brazil are presented. The daily cross-correlations were stacked using a timefrequency, phase-weighted scheme that enhances weak coherent signals by reducing incoherent noise. The cross-correlations show that, as expected, the emerged signal is dominated by Rayleigh waves, with dispersion velocities being reliably measured for periods ranging between 5 and 20 s. Both permanent stations from a monitoring seismic network and temporary stations from past passive experiments in the region are considered, resulting in a combined network of 33 stations separated by distances between 60 and 1311 km, approximately. The Rayleigh-wave, dispersion velocity measurements are then used to develop tomographic images of group velocity variation for the Borborema Province of Northeast Brazil. The tomographic maps allow to satisfactorily map buried structural features in the region. At short periods (~5 s) the images reflect shallow crustal structure, clearly delineating intra-continental and marginal sedimentary basins, as well as portions of important shear zones traversing the Borborema Province. At longer periods (10 – 20 s) the images are sensitive to deeper structure in the upper crust, and most of the shallower anomalies fade away. Interestingly, some of them do persist. The deep anomalies do not correlate with either the location of Cenozoic volcanism and uplift - which marked the evolution of the Borborema Province in the Cenozoic - or available maps of surface heat-flow, and the origin of the deep anomalies remains enigmatic.

Avaliação do controle da diagênese na qualidade de reservatório siliciclástico do cenomaniano superior da formação Açu, sudoeste da bacia potiguar

The distribution of diagenetic alterations in Late Cenomanian siliciclastic reservoirs from Potiguar Basin was influenced by the stratigraphic framework and the depositional system. Seismic sections and geophysical logs of two wells drilled in the SW portion of the mentioned basin above register regional stratigraphic surfaces representing maximum floods related to a transgressive event. The sequential analysis of 80 m of drill core (~450 m deep) recognized nine depositional facies with an upwards granodecrescent standard piling that limits cycles with an erosional conglomeratic base (lag) overlain by intercalations of medium to very fine sandstones showing cross bedding (channel, planar and low angled) and horizontal bedding (plane-parallel , wave and flaser). The top of the cycles is marked by the deposition of pelites and the development of paleosoils and lagoons. The correlation of genetically related facies reveals associations of channel fillings, crevasse, and flood plains deposited in a transgressive system. Detailed descriptions of seventy nine thin sections aided by MEV-EBSD/EDS, DRX and stable isotope analyses in sandstones revealed an arcosian composition and complex textural arrays with abundant smectite fringes continuously covering primary components, mechanically infiltrated cuticles and moldic and intragrain pores. K-feldspar epitaxial overgrowth covers microcline and orthoclase grains before any other phase. Abundant pseudomatrix due to the compactation of mud intraclasts concentrate along the stratification planes, locally replaced by macrocristalline calcite and microcrystalline and framboidal pyrite. Kaolinite (booklets and vermicular), microcrystalline smectite, microcrystalline titanium minerals and pyrite replace the primary components. The intergrain porosity prevails over the moldic, intragrain and contraction porosities. The pores are poorly connected due to the presence of intergranular smectite, k-feldspar overgrowth, infiltrated mud and pseudomatrix. The sandstones were subjected to eodiagenetic conditions next to the surface and shallow burial mesodiagenetic conditions. The diagenetic alterations reduced the porosity and the permeability mainly due to the precipitation of smectite fringes, compactation of mud intraclasts onto the pseudomatrix and cementing by poikilotopic calcite characterizing different reservoir petrofacies. These diagenetic products acted as barriers and detours to the flow of fluids thus reducing the quality of the reservoir.

Medium change monitoring using ambient seismic noise and coda wave interferometry: examples from intraplate NE Brazil and the Mid-Atlantic Ridge

This thesis presents and discusses the results of ambient seismic noise correlation for two different environments: intraplate and Mid-Atlantic Ridge. The coda wave interferometry method has also been tested for the intraplate data. Ambient noise correlation is a method that allows to retrieve the structural response between two receivers from ambient noise records, as if one of the station was a virtual source. It has been largely used in seismology to image the subsurface and to monitor structural changes associated mostly with volcanic eruptions and large earthquakes. In the intraplate study, we were able to detect localized structural changes related to a small earthquake swarm, which main event is mR 3.7, North-East of Brazil. We also showed that the 1-bit normalization and spectral whitening result on the loss of waveform details and that the phase auto-correlation, which is amplitude unbiased, seems to be more sensitive and robust for our analysis of a small earthquake swarm. The analysis of 6 months of data using cross-correlations detect clear medium changes soon after the main event while the auto-correlations detect changes essentially after 1 month. It could be explained by fluid pressure redistribution which can be initiated by hydromechanical changes and opened path ways to shallower depth levels due to later occurring earthquakes. In the Mid-Atlantic Ridge study, we investigate structural changes associated with a mb 4.9 earthquake in the region of the Saint Paul transform fault. The data have been recorded by a single broadband seismic station located at less than 200 km from the Mid-Atlantic ridge. The results of the phase auto-correlation for a 5-month period, show a strong co-seismic medium change followed by a relatively fast post-seismic recovery. This medium change is likely related to the damages caused by the earthquake’s ground shaking. The healing process (filling of the new cracks) that lasted 60 days can be decomposed in two phases, a fast recovery (70% in ~30 days) in the early post-seismic stage and a relatively slow recovery later (30% in ~30 days). In the coda wave interferometry study, we monitor temporal changes of the subsurface caused by the small intraplate earthquake swarm mentioned previously. The method was first validated with synthetics data. We were able to detect a change of 2.5% in the source position and a 15% decrease of the scatterers’ amount. Then, from the real data, we observed a rapid decorrelation of the seismic coda after the mR 3.7 seismic event. This indicates a rapid change of the subsurface in the fault’s region induced by the earthquake.

Medium change monitoring using ambient seismic noise and coda wave interferometry: examples from intraplate NE Brazil and the Mid-Atlantic Ridge

This thesis presents and discusses the results of ambient seismic noise correlation for two different environments: intraplate and Mid-Atlantic Ridge. The coda wave interferometry method has also been tested for the intraplate data. Ambient noise correlation is a method that allows to retrieve the structural response between two receivers from ambient noise records, as if one of the station was a virtual source. It has been largely used in seismology to image the subsurface and to monitor structural changes associated mostly with volcanic eruptions and large earthquakes. In the intraplate study, we were able to detect localized structural changes related to a small earthquake swarm, which main event is mR 3.7, North-East of Brazil. We also showed that the 1-bit normalization and spectral whitening result on the loss of waveform details and that the phase auto-correlation, which is amplitude unbiased, seems to be more sensitive and robust for our analysis of a small earthquake swarm. The analysis of 6 months of data using cross-correlations detect clear medium changes soon after the main event while the auto-correlations detect changes essentially after 1 month. It could be explained by fluid pressure redistribution which can be initiated by hydromechanical changes and opened path ways to shallower depth levels due to later occurring earthquakes. In the Mid-Atlantic Ridge study, we investigate structural changes associated with a mb 4.9 earthquake in the region of the Saint Paul transform fault. The data have been recorded by a single broadband seismic station located at less than 200 km from the Mid-Atlantic ridge. The results of the phase auto-correlation for a 5-month period, show a strong co-seismic medium change followed by a relatively fast post-seismic recovery. This medium change is likely related to the damages caused by the earthquake’s ground shaking. The healing process (filling of the new cracks) that lasted 60 days can be decomposed in two phases, a fast recovery (70% in ~30 days) in the early post-seismic stage and a relatively slow recovery later (30% in ~30 days). In the coda wave interferometry study, we monitor temporal changes of the subsurface caused by the small intraplate earthquake swarm mentioned previously. The method was first validated with synthetics data. We were able to detect a change of 2.5% in the source position and a 15% decrease of the scatterers’ amount. Then, from the real data, we observed a rapid decorrelation of the seismic coda after the mR 3.7 seismic event. This indicates a rapid change of the subsurface in the fault’s region induced by the earthquake.

Desenvolvimento de um exoesqueleto para movimentação/reabilita-ção de paraplégicos

People bedridden by paralysis/motor disability are subject to several problems due to lack of movement. Then, it is necessary to use equipments that enable the people bedridden stand up and walk, so as to reduce the problems due to lack of movement and the time of rehabilitation, impacting directly on its quality of life. The aim of this work is the development of an exoskeleton to make the movement of people with paralysis / motor impairment in the lower limbs, without help of third parties, to be activated by the user. To provide support, stability and security to the deficient, it was decided to use a structure formed by four legs, being each leg consisting of a parallel chain. The gait was obtained by combining the movement of two mechanisms: crank/rocker, responsible for oscillatory motion of the leg, and cam/follower, responsible for the foot motion on the desired trajectory. To achieve the aim of this work was conducted a study about the types of exoskeletons for locomotion/rehabilitation of people with lower limb paralysis and presented a study on the movement of the lower limb joints. It also presented a mathematical model to obtain the desired path to the foot of the exoskeleton, the static model and the design of the structure elements. In the sequence is presented the simulation of movements of a people during the human gait, experimental tests and the comparison with the human gait developed by a people without disabilities.

Impulsão horizontal de futebolistas da segunda divisão do campeonato gaúcho

No futebol a impulsao tem impacto no cabeceio, nos movimentos de antecipaçoes, nos diferentes saltos e de forma geral, na velocidade das açoes de jogo. No entanto, ao contrário de outros esportes como Basquete, Vôlei, Handebol, o seu treinamento específico é pouco visado no futebol. O objetivo deste estudo é verificar, em atletas profissionais de futebol de campo, o perfil da impulsao horizontal e o desenvolvimento dessa durante uma temporada de treinamento e jogos pela segunda divisao do campeonato gaúcho. Foram avaliados 18 atletas de futebol (com média de idade 25±5,44 anos, altura 177,5±6,48 cm e massa corporal 79,4±9,67 kg). Os atletas se submeteram a testes de impulsao horizontal no início (pré) e após três meses de treinamentos (pós). Mediu-se os saltos com ambas às pernas, cinco saltos consecutivos com membro direito (MID) e esquerdo (MIE) e cinco saltos alternados. O perfil de impulsao obtido no pré-teste foi respectivamente 2,22±0,14m, 11,46±0,56 m, 11,69±0,73m e 12,04±0,78m. Os resultados do pós-teste nao se alteraram em comparaçao ao primeiro teste, sendo respectivamente 2,22±0,15m, 11,26±1,12m, 11,46±0,95m e 12,02±0,76m. Conclui-se que o treinamento nao foi capaz de proporcionar desenvolvimento desta capacidade, pois predominantemente as rotinas de treinamento de futebol nao enfocam este desenvolvimento

Impulsão horizontal de futebolistas da segunda divisão do campeonato gaúcho

No futebol a impulsao tem impacto no cabeceio, nos movimentos de antecipaçoes, nos diferentes saltos e de forma geral, na velocidade das açoes de jogo. No entanto, ao contrário de outros esportes como Basquete, Vôlei, Handebol, o seu treinamento específico é pouco visado no futebol. O objetivo deste estudo é verificar, em atletas profissionais de futebol de campo, o perfil da impulsao horizontal e o desenvolvimento dessa durante uma temporada de treinamento e jogos pela segunda divisao do campeonato gaúcho. Foram avaliados 18 atletas de futebol (com média de idade 25±5,44 anos, altura 177,5±6,48 cm e massa corporal 79,4±9,67 kg). Os atletas se submeteram a testes de impulsao horizontal no início (pré) e após três meses de treinamentos (pós). Mediu-se os saltos com ambas às pernas, cinco saltos consecutivos com membro direito (MID) e esquerdo (MIE) e cinco saltos alternados. O perfil de impulsao obtido no pré-teste foi respectivamente 2,22±0,14m, 11,46±0,56 m, 11,69±0,73m e 12,04±0,78m. Os resultados do pós-teste nao se alteraram em comparaçao ao primeiro teste, sendo respectivamente 2,22±0,15m, 11,26±1,12m, 11,46±0,95m e 12,02±0,76m. Conclui-se que o treinamento nao foi capaz de proporcionar desenvolvimento desta capacidade, pois predominantemente as rotinas de treinamento de futebol nao enfocam este desenvolvimento