53 resultados para Cartografia


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Cartographical representations (maps, charters and plans) are taken as didactic resources in Geography classes in the 5th grade of the municipal public schools in São José de Ribamar through a methodological approach taking into consideration the use of those resources is still worries an important part of the teachers of the Maranhão State public schools who teach in this level. Papers related to the theme, most of the time, are non accessible to the teachers of the maranhense public schools, mainly because the education instilutions, which use those resources, do it in a very incipient way. So this research proposes from the drawings of magnetccoursein the school courtyards, together with maps, charts, plans among others representation used in the classroom environment, motivate the students to a deeper interests in participating in Geography learning process in the 5th grade. Interviews, analyses of socialcultural questionnaires of the families involved in the process; observations of classes, trainings, geocartographical orientations, application of pre and posttests, discussions about the usage of cartographic representations, proposed and effectivated tasks in the classroom, as well as around the school, were the basis of the researched population. As a result of this process, it was produced a was complement didatical material showing, among others, the space in which students, for sure, will contribute in an effective way to a better teaching practice in the chain of maranhense public schools, having in mind that these geographic subjects may be taught in the level we focused our study

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The crisis of the model of technical and formal rationality is discussed in light of a paradigmatic change of the Law that arises in the context of recent transformations of capitalism worldwide, proposing a humanization of Law and Justice with a new ethical-political foundation that promotes a reconciliation between the rules that governs the social order and the world of life, a process of society’s emancipation. As empirical cut it is taken the Right of Children and Youth and, in a practical perspective, the recognition and effectiveness of the Rights of Children and Adolescents in Brazil. It is proposed to analyze the process of democratization and legitimacy of the children and youth rights from the study and apprehension of knowledge that advocate a multidisciplinary view of knowledge and a dialogic praxis for construction of a thought able to contribute to the analysis of public policies and to develop strategies that allow a real change on the social thinking about the doctrine of integral protection of children and adolescents. The proposed methodological approach was developed from a dialectical view of science and as a research strategy for data collection of symbolic cartography or cartographic sociology of law and justice. It is shown that in the process of humanization of the Law and Justice there is a gap between the rights and the democratic participation of these rights.

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The indigenous political scene in Brazil is undergoing transformations that need to be better analyzed by scholars in the field of the Social Sciences. The deficit in the policy of indigenous land demarcation emerges as the largest obstacle in the conquest of collective rights. Therefore, a study to analyze renewed strategies in the struggle for social rights, and their implications in local everyday life relations, is urgent. In this context, the aim of this research is to understand the current social dynamics of identity among the Tremembé people of Almofala, in the state of Ceará, Brazil, with a fieldwork conducted in the flour mill of the Casa de Farinha Comunitária project, in the Lameirão community. Specific aims are: a) to analyze the processes involved in the project in order to comprehend their meanings and appropriations as well as their everyday life and political uses; b) understand the strategies to fight for social benefits; c) analyze the local ethnic classifications grounding the construction of the Tremembé identity in Almofala. Methods deployed are ethnography of communities, used to apprehend the social production of networks of relationships, and a social cartography of practices. The realization of rights demanded by the indigenous populations in Brazil is intertwined with a process of social and legal legitimation their identity and cultural heritage. Such legitimation works as a safeguard mechanism of rights secured by the Constitution. Therefore, to own a “cultural heritage” is perceived as a “passport” to benefit from emerging rights. Amid this context, changes in the traditional processing of the cassava root, a productive practice shared locally by diverse social groups, is reified as cultural heritage by the Tremembé people of Almofala and their network of collaborators in the pursuit of accessing distinctive public policies. Furthermore, the research came across specific social arrangements of local subjects which unfolded internal struggles, enabling to understand the dynamics of the Tremembé of Almofala identity process.

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPES

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The present paper discusses the experience of a psychological emergency attendance in Maternidade Escola Januário Cicco (MEJC) in Natal and has as main objective to investigate the limits and possibilities of this practice in offering psychological care to women in abortion situation. The Ministry of Health considers the abortion a serious medical problem in Brazil and acknowledge the repercussions it causes in personal life and between the women’s family, most of all among the younger ones, in fully productive and reproductive age, that if not supported may suffer deep psychological and physical wounds. This research inserts itself in the field of psychological practices in institutions, by many ways, and aim to offer, by different approaches, among then the psychological emergency attendance, a psychological attention at the institutions. This attention refers to a care during the suffering at the time of crisis and in the many ways that the problem is present. The results were analyzed at a heideggerian hermeneutics optics, which search a determined aspect of reality that intends to know/understand, accompanied by the man’s own movement in existence. The cartography and the logbook were chosen in narrative form as a resource to allow the approximation of daily experience. The emergency psychological attendance was realized on curettage setor of MEJC between march of 2013 and february 2014 at tuesdays and Thursdays from 9h to 12h. The existential plot unveiled at this experience showed some possibilities and limits of emergency psychological attendance as studied. Among the possibilities, the emergency attendance helped the women that suffered an abortion to find new meanings, as: realize the need to self-care; see in the attendance a way to cope with the lost or other issues in their life’s; to enlarge the possibilities of her choice; to rethink her sex e reproductive life, and rethink her relationships and life projects. The attendance has proven itself as a health care mechanism showing the women the need to search for the necessary condition to self-care and to question what in that environment was saw as natural. The attendance showed itself as a suitable practice to the health care demand by creating/inventing ways of meet the woman needs. The attendance promoted an opening at the technical horizons of women’s, what was realized when the complaints moved past the physical health. As refered to the limits, some needs was beyond the emergency attendance service and demanded forwarding to regular psychological care or others specialized services. The service was not able to attend all of the demands of the sector. The attendance did not touched the medical staff to its need or made a change in posture to act beyond the technicality. The attendance, although has not made change in this context, was able to show the main difficulties, like the lack on prepare of the medical staff to deal with the abortion past beyond the technical procedure and the precariousness of the infrastructure of the services offered. At last, the attendance represented a shelter to the women in abortion situation, allowing the suffering to have a place.

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The ediacaran plutonic activity related to the Brasilian/Pan-African orogeny is one of the most important geological features in the Borborema Province, represented along its extension by numerous batholiths, stocks, and dikes.The object of this study, the Serra Rajada Granitic Pluton (SRGP), located in the central portion of the Piranhas-Seridó River Domain is an example of this activity. This pluton has been the subject of cartographic, petrographic, geochronological and lithogeochemical studies and its rocks were characterized by two facies. First, the granitic facies were described as monzogranites consisting of K-feldspar, plagioclase (oligoclase - An23-24%), quartz and biotite (main mafic) and opaque minerals such as titanite, allanite, apatite, and zircon as accessories. Alteration minerals are chlorite, white mica and carbonate. Second, the dioritic facies consist of rocks formed by quartz diorite containing plagioclase (dominant mineral phase), quartz and K-feldspar. Biotite and amphibole are the dominant mafic minerals; and titanite, opaque minerals, allanite, zircon and apatite are the accessories. However, previous geological mapping work in the region also identified the presence of other lithostratigraphic units. These were described as gneisses and migmatites with undifferentiated amphibolite lenses related to the Caicó Complex (Paleoproterozoic) and metasedimentary rocks of the Seridó Group (Neoproterozoic) composed of paragneiss with calc-silicate lenses, muscovite quartzite and biotite schist (respectively, the Jucurutu formations, Equador and Seridó), the host rocks for the SRGP rocks. Leucomicrogranite and pegmatite dikes have also been identified, both related to the end of the Ediacaran magmatism and colluvial- eluvial and alluvial deposits related to Neogene and Quaternary, respectively. Lithogeochemical data on the SRGP granite facies, highlighted quite evolved rocks (SiO2 69% to 75%), rich in alkalis (Na2O+K2O ≥ 8.0%), depleted of MgO (≤ 0.45%), CaO (≤ 1.42%) and TiO2 (≤ 0.36%) and moderate levels of Fe2O3t (2.16 to 3.53%). They display transitional nature between metaluminous and peraluminous (predominance of the latter) with sub-alkaline/monzonitic (High K calcium-alkali) affinity. Harker diagrams show negative correlations for Fe2O3t, MgO, and CaO, indicating mafic and plagioclase fractionation. REE spectrum shows enrichment of LREE relative to heavy REE (LaN/YbN = 23.70 to 10.13), with negative anomaly in the Eu (Eu/Eu* = 0.70 to 0.23), suggesting fractionation or accumulation in the feldspars source (plagioclase). Data integration allows to correlate the SRGP rocks with those described as Calcium-Alkaline Suite of equigranular High K. The crystallization conditions of the SRGP rocks were determined from the integration of petrographic and lithogeochemical data. These data indicated intermediate to high conditions of ƒO2 (mineral paragenesis titanite + magnetite + quartz), parent magma saturated in H2O (early biotite crystallization), tardi-magmatic processes of fluids rich in ƒCO2, H2O and O2 causing part of the mineral assembly to change (plagioclase carbonation and saussuritization, biotite chloritization and opaques Sphenitization). Thermobarometrical conditions were estimated based on geochemical parameters (Zr and P2O5) and CIPW normative minerals, with results showing the liquidus minimum temperature of about800°C and the solidus temperature of approximately 700°C. The final/minimum crystallization pressure are suggested to be between 3 and 5 Kbar. The presence of zoned minerals (plagioclase and allanite) associated with lithogeochemical data in bi-log diagrams for Rb vs. Ba and Rb vs. Sr suggest the role of fractional crystallization as the dominant process in the magmatic evolution of SRGP. U-Pb Geochronological and Sm-Nd isotope studies indicated, respectively, the crystallization age of biotite monzogranite as 557 ± 13 Ma, with TDM model age of 2.36 Ga, and εNd value of -20.10 to the crystallization age, allowing to infer paleoproterozoic crustal source for the magma.

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The ediacaran plutonic activity related to the Brasilian/Pan-African orogeny is one of the most important geological features in the Borborema Province, represented along its extension by numerous batholiths, stocks, and dikes.The object of this study, the Serra Rajada Granitic Pluton (SRGP), located in the central portion of the Piranhas-Seridó River Domain is an example of this activity. This pluton has been the subject of cartographic, petrographic, geochronological and lithogeochemical studies and its rocks were characterized by two facies. First, the granitic facies were described as monzogranites consisting of K-feldspar, plagioclase (oligoclase - An23-24%), quartz and biotite (main mafic) and opaque minerals such as titanite, allanite, apatite, and zircon as accessories. Alteration minerals are chlorite, white mica and carbonate. Second, the dioritic facies consist of rocks formed by quartz diorite containing plagioclase (dominant mineral phase), quartz and K-feldspar. Biotite and amphibole are the dominant mafic minerals; and titanite, opaque minerals, allanite, zircon and apatite are the accessories. However, previous geological mapping work in the region also identified the presence of other lithostratigraphic units. These were described as gneisses and migmatites with undifferentiated amphibolite lenses related to the Caicó Complex (Paleoproterozoic) and metasedimentary rocks of the Seridó Group (Neoproterozoic) composed of paragneiss with calc-silicate lenses, muscovite quartzite and biotite schist (respectively, the Jucurutu formations, Equador and Seridó), the host rocks for the SRGP rocks. Leucomicrogranite and pegmatite dikes have also been identified, both related to the end of the Ediacaran magmatism and colluvial- eluvial and alluvial deposits related to Neogene and Quaternary, respectively. Lithogeochemical data on the SRGP granite facies, highlighted quite evolved rocks (SiO2 69% to 75%), rich in alkalis (Na2O+K2O ≥ 8.0%), depleted of MgO (≤ 0.45%), CaO (≤ 1.42%) and TiO2 (≤ 0.36%) and moderate levels of Fe2O3t (2.16 to 3.53%). They display transitional nature between metaluminous and peraluminous (predominance of the latter) with sub-alkaline/monzonitic (High K calcium-alkali) affinity. Harker diagrams show negative correlations for Fe2O3t, MgO, and CaO, indicating mafic and plagioclase fractionation. REE spectrum shows enrichment of LREE relative to heavy REE (LaN/YbN = 23.70 to 10.13), with negative anomaly in the Eu (Eu/Eu* = 0.70 to 0.23), suggesting fractionation or accumulation in the feldspars source (plagioclase). Data integration allows to correlate the SRGP rocks with those described as Calcium-Alkaline Suite of equigranular High K. The crystallization conditions of the SRGP rocks were determined from the integration of petrographic and lithogeochemical data. These data indicated intermediate to high conditions of ƒO2 (mineral paragenesis titanite + magnetite + quartz), parent magma saturated in H2O (early biotite crystallization), tardi-magmatic processes of fluids rich in ƒCO2, H2O and O2 causing part of the mineral assembly to change (plagioclase carbonation and saussuritization, biotite chloritization and opaques Sphenitization). Thermobarometrical conditions were estimated based on geochemical parameters (Zr and P2O5) and CIPW normative minerals, with results showing the liquidus minimum temperature of about800°C and the solidus temperature of approximately 700°C. The final/minimum crystallization pressure are suggested to be between 3 and 5 Kbar. The presence of zoned minerals (plagioclase and allanite) associated with lithogeochemical data in bi-log diagrams for Rb vs. Ba and Rb vs. Sr suggest the role of fractional crystallization as the dominant process in the magmatic evolution of SRGP. U-Pb Geochronological and Sm-Nd isotope studies indicated, respectively, the crystallization age of biotite monzogranite as 557 ± 13 Ma, with TDM model age of 2.36 Ga, and εNd value of -20.10 to the crystallization age, allowing to infer paleoproterozoic crustal source for the magma.

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Tanto no contexto acadêmico quanto no artístico e mercadológico, é crescente a discussão sobre o espaço de conceituação da dança contemporânea e suas fissuras, que deixam de abarcar esta ou aquela manifestação artística ou mesmo acaba por abarcar aquelas manifestações que não se encaixam em outros espaços de conceituação. No presente trabalho objetivamos a investigar, a Dança na Contemporaneidade, para além do que se entende por dança contemporânea, em sua capacidade de atravessar os espaços de conceituação já estabelecidos, para implicar em uma pluralidade de fazeres. Objetivamos também pensar a potência que a Dança imprime no corpo do artista criador, pensando também como este se comporta no espaço de entre linguagens . A dissertação que aqui se apresenta encontrou enquanto estratégia metodológica o recurso da metáfora, partindo das ideias de travessia, cartografia e cidades invisíveis para a construção do pensamento sobre o corpo do artista e suas relações com as diferentes linguagens artísticas, tomando por base uma retomada das experiências estéticas e artísticas de sua proponente. Dialogando experiências práticas e referenciais teóricos, inicialmente tratamos da dança contemporânea em seus problemas de classificação que apontam para a necessidade de um pensamento contemporâneo em dança, que pense as manifestações artísticas em seus pontos convergentes, e não nos divergentes que as situam sob diversas nomenclaturas. No capítulo seguinte discutimos a possibilidade de contaminação entre as linguagens artísticas a partir do próprio corpo-artista. Discorremos também sobre a dança enquanto agenciamento e resposta aos impulsos resultantes da relação com o espaço e outros corpos, pensando como o corpo do vivente se organiza nesta relação de compartilhamento de experiências. Mostrando uma potência do corpo artista criador que se dedica à transvaloração das fronteiras entre as linguagens para a organização do seu fazer. Por fim, apontamos para a diversidade na metodologia de processos de criação que variam de acordo com as possibilidades técnicas e necessidades estéticas de cada artista criador