Terceirização versus agenda do trabalho decente : estudo de caso a partir do Banco do Brasil s.a. na Paraíba

This Dissertation examines outsourcing in Bank of Brazil SA, the state of Paraiba. The central research question is to what extent this flexibility of labor relations incorporates items claimed by ´recent´ Decent Work Agenda of the International Labour Organization (OIT) or, on the contrary, the ´epidemic´ of outsourcing makes it even more challenging the world of work in the third millennium. The research hypothesis is that the Bank of Brazil has a growing subcontracting / outsourcing of labor (companies and individuals) and that not only contributes to the deterioration of working conditions, but also opposes the Work Agenda decent. Aiming to prove or disprove the hypothesis, the study includes a survey and secondary field. The literature review focuses on the trend towards casualization of labor in capitalism, and yet, in an effort to systematize data and analysis on ´outsourcing´ from the viewpoint of different actors. This theoretical framework is anchored in important classical sources and present that address the topic in the world and in Brazil. The field research was conducted with the actors related to the theme of ´outsourcing´ the Bank of Brazil - Paraiba, precisely branch managers, permanent employees of the bank, union representatives (bank workers), union bank and outsourced. The results confirm, in part, the study hypothesis, by demonstrating that there are several meanings and forms of precariousness that the contractors surveyed are submitted, highlighting the issue of salaries, the work environment, union representation and health worker. All these themes, each for himself, are contemplated by the Decent Work Agenda of the ILO and show, according to field research, rather fragile

Condicionamento estrutural das zonasa de cisalhamento da região de Forquilha, domínio Ceará Central: uma abordagem integrada de sensoriamento remoto e geologia estrutural

The studied region, named Forquilha and localized in northwestern Central Ceará domain (northern portion of Borborema Province), presents a lithostratigraphic framework constituted by paleoproterozoic metaplutonics, metasedimentary sequences and neoproterozoic granitoids. The metasedimentary rocks of Ceará group occupy most part of the area. This group is subdivided in two distinct units: Canindé and Independência. Canindé unit is represented basically by biotite paragneisses and muscovite paragneisses, with minor metabasic rocks (amphibolite lens). Independência sequence is composed by garnetiferous paragneisses, sillimanite-garnet-quartz-muscovite schists and quartz-muscovite schists, pure or muscovite quartzites and rare marbles. At least three ductile deformation events were recognized in both units of Ceará group, named D1, D2 and D3. The former one is interpreted as related to a low angle tangential tectonics which mass transport is southward. D2 event is marked by the development of close/isoclinal folds with a N-S oriented axis. Refolding patterns generated by F1 and F2 superposition are found in several places. The latest event (D3) corresponds to a transcurrent tectonics, which led to development of mega-folds and several shear zones, under a transpressional regime. The mapped shear zones are Humberto Monte (ZCHM), Poço Cercado (ZCPC) and Forquilha (ZCF). Digital image processing of enhanced Landsat 7-ETM+ satellite images, combined with field data, demonstrate that these penetrative structures are associated with positive and negative geomorphologic patterns, distributed in linear and curvilinear arrangements with tonal banding, corresponding to the ductile fabric and to crests. Diverse color composites were tested and RGB-531 and RGB-752 provided the best results for lineament analysis of the most prominent shear zones. Spatial filtering techniques (3x3 and 5x5 filters) were also used and the application of Prewitt filters generated the best products. The integrated analysis of morphological and textural aspects from filtered images, variation of tonalities related to the distribution of geologic units in color composites and the superposition over a digital elevation model, contributed to a characterization of the structural framework of the study area. Kinematic compatibility of ZCHM, ZCPC, ZCF shear zones, as well as Sobral-Pedro II (ZCSPII) shear zone, situated to the west of the study area, was one of the goal of this work. Two of these shear zones (ZCHM, ZCPC) display sinistral movements, while the others (ZCSPII, ZCF) exhibit dextral kinematics. 40Ar/39Ar ages obtained in this thesis for ZCSPII and ZCPC, associated with other 40Ar/39Ar data of adjacent areas, indicate that all these shear zones are related to Brasiliano orogeny. The trend of the structures, the opposite shear senses and the similar metamorphic conditions are fitted in a model based on the development of conjugate shear zones in an unconfined transpression area. A WNW-ESE bulk shortening direction is infered. The geometry and kinematic of the studied structures suggest that shortening was largely accommodated by lateral extrusion, with only minor amounts of vertical stretch