937 resultados para East and West.
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The study area of the Guarda-Mor target (Israelândia-GO) contextualizes the terrains of the estaern portion of the Arenópolis Magmatic Arc, more accurately, the Neoproterozoic associations inserted in the field of the Jaupaci volcano-sedimentary sequence. The mapped area is located in the central-western of Goiás state. The presente paper has as main objective to characterize the structural, petrographic and litogeochemistry of the target rocks beyond to compare these factors with the Mina Bacilândia rocks (Fazenda Nova-GO) in order to assess the genetic similarity of volcano-sedimentary units and deposits associated. The Guarda-Mor target is represented by the Jaupaci metavolcanic rocks sequence presenting bimodal volcanism. This sequence consists in metafelsic rocks like sericite/muscovite quartz schist, phyllite and metarriolites and/or metariodacites with calc-alkaline geochemical signature and metamafic rocks with tholeiitic character formed by actinolite - chlorite schist and chlorite - quartz schist. Besides the package of supracrustal rocks also can be observed the occurrence of a local intrusion syn- to late - tectonic named Granito Subvulcânico. In the study area beyond the marked volcanism also seen an event of crustal melting granitogênese evidenced by the presence of 2 granites at the east and the west of the map, Granito Israelândia and Granito Iporá respectively. Structural analysis both at the macro and micro have identified 3 deformation phases. The types of rock on the region record features in the metamorphic facies top and down. These features were subdivided into 3 metamorphic areas: the east and West areas show thermal metamorphism due to intrusion of adjacente granites while the central domain displays features of regional metamorphism. Gold mineralization of the Guarda –Mor deposit target suggests a possible structural control beyond pronounced the hydrothermal alteration. The mineralization may also be...
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Pós-graduação em Agronomia (Ciência do Solo) - FCAV
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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
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[EN]This dissertation analyses the Eastern cultural influences present in the aesthetic of Buck’s best seller The Good Earth. The objective is to study the characteristics of Buck’s aesthetic as a product of a creative process of self-translation between Mandarin and English. The methodology of analysis has focused on the characters of the novel, the strategies used to refer to them, the characters’ idiolect and their social interaction (facework). Finally, these cultural aspects have been compared with one of the Spanish translations available of the novel. The results obtained show a novel highly influenced by the Eastern tradition, where the idiolect of the characters show an influence from both East and West possible thanks to the mechanism of self-translation.
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Lava aus der quartären Vulkanregion der Eifel wurde in römischer Zeit großmaßstäblich abgebaut, um daraus Mühlsteine hoher Qualität herzustellen, die in großen Mengen in weite Teile des Römischen Reiches exportiert wurden. Somit erweisen sich diese Mühlsteine als ideale Indikatoren für Handelsgebiete und –wege dieser Zeit. Für eine erfolgreiche Herkunftsanalyse von Fundstücken ist eine genaue Charakterisierung der infrage kommenden Rohstoffe die unbedingte Voraussetzung. Aus diesem Grund konzentriert sich diese Arbeit auf die geochemische Definition der 16 bekannten römischen „Basalt“-Abbaustellen in den Vulkanfeldern der Ost- und Westeifel, mit dem vorrangigen Ziel, eine möglichste eindeutige Charakterisierung der einzelnen Abbaustellen zu erreichen. Auf dieser Basis wird eine Vorgehensweise zur folgenden Provenienzanalyse der Mühlsteine entwickelt. Um die geochemische Variabilität der Laven zu erfassen wurden die Abbaustellen großflächig beprobt. Die Proben wurden zunächst petrographisch bestimmt und der Phasenbestand mittels Röntgendiffraktometrie (XRD) untersucht. Die Haupt- und Spurenelement-Zusammensetzung wurde anhand von Röntgenfluoreszenzanalysen und Laser-Massenspektrometrie mit induktiv gekoppeltem Plasma (LA-ICP-MS) ermittelt, die Sr-Nd-Pb-Isotopie ausgewählter Proben mittels Thermo-Ionen-Massenspektrometrie (TIMS). Es zeigte sich, dass auf Grundlage der Haupt- und Spurenelementzusammensetzung, gemessen mit RFA, eine Abgrenzung der Abbaustellen zueinander mittels einer Kombination aus geochemischer Diskriminierung mit Cluster- und Diskriminanzanalysen gelingt. Die anschließende Provenienzanalyse der Mühlsteinfundstücke erfolgt analog zur Charakterisierung der Abbaustellen. Im ersten Schritt wird eine geochemische Zuordnung des Fundstücks vorgenommen, um zu überprüfen, ob eine Eifeler Herkunft überhaupt in Frage kommt. Lässt der geochemische Vergleich mit den Referenzdaten aus dem Gelände eine Eifeler Herkunft zu, kommt im zweiten Schritt die Clusteranalyse zum Einsatz. Hier wird auf multivariater Ebene geprüft, ob das Fundstück einer Eifeler Abbaustelle oder einem Cluster von Eifeler Abbaustellen zugeordnet werden kann. Bei einer positiven Zuordnung wird ergänzend als dritter Schritt die Diskriminanzanalyse angewendet, anhand der das Mühlstein-Fundstück einer Abbaustelle mit einer bestimmten Wahrscheinlichkeit zugewiesen wird. Bei 68 analysierten Mühlsteinen aus verschiedenen Regionen Mitteleuropas konnte so für 49 Fundstücke eine Eifeler Provenienz festgestellt werden. Alle römischen Eifeler Mühlsteine entstammen dem Bellerberg bei Mayen, ein mittelalterliches Stück aus dem Niedermendiger Lavastrom. Die Zuordnung der übrigen 19 Mühlsteine zu anderen möglichen Abbaugebieten erfolgt anhand geochemischer Daten aus der Literatur. Aufgrund der unzureichenden Datenlage sind im Falle dieser Proben jedoch im Gegensatz zur Lavastrom-genauen Zuordnung der Eifeler Mühlen lediglich Vermutungen über die Herkunftsregionen möglich. Damit zeigt sich, dass eine ausführliche Referenzdatenbank der in Frage kommenden Rohstoffe die erforderliche Basis für erfolgreiche Provenienzanalysen ist. Die Möglichkeit der genauen Zuordnungen von Mühlsteinen zu den Eifeler Abbaustellen belegt, dass die Verbindung von geochemischer Auswertung mit Cluster- und Diskriminanzanalysen ein hilfreiches Verfahren zur Provenienzanalyse darstellt.
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Tra il V ed il VI secolo, la città di Ravenna, per tre volte capitale, emerge fra i più significativi centri dell’impero, fungendo da cerniera tra Oriente e Occidente, soprattutto grazie ai mosaici parietali degli edifici di culto, perfettamente inseriti in una koinè culturale e artistica che ha come comune denominatore il Mar Mediterraneo, nel contesto di parallele vicende storiche e politiche. Rispetto ai ben noti e splendidi mosaici ravennati, che insieme costituiscono senza dubbio un unicum nel panorama artistico dell’età tardoantica e altomedievale, nelle decorazioni musive parietali dei coevi edifici di culto dei diversi centri dell’impero d’Occidente e d’Oriente, e in particolare in quelli localizzati nelle aree costiere, si possono cogliere divergenze, ma anche simmetrie dal punto di vista iconografico, iconologico e stilistico. Sulla base della letteratura scientifica e attraverso un poliedrico esame delle superfici musive parietali, basato su una metodologia interdisciplinare, si è cercato di chiarire l’articolato quadro di relazioni culturali, ideologiche ed artistiche che hanno interessato e interessano tuttora Ravenna e i vari centri della tarda antichità, insistendo sulla pluralità, sulla complessità e sulla confluenza di diverse esperienze artistiche sui mosaici di Ravenna. A tale scopo, i dati archeologici e artistici sono stati integrati con quelli storici, agiografici ed epigrafici, con opportuni collegamenti all’architettura, alla scultura, alle arti decorative e alle miniature, a testimonianza dell’unità di intenti di differenti media artistici, orientati, pur nella diversità, verso le medesime finalità dogmatiche, politiche e celebrative. Si tratta dunque di uno studio di revisione e di sintesi sui mosaici parietali mediterranei di V e VI secolo, allo scopo di aggiungere un nuovo tassello alla già pur vasta letteratura dedicata all’argomento.
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Il presente lavoro di ricerca si focalizza sulla rappresentazione della cultura arabo-islamica, così come viene restituita nei libri di storia per la scuola secondaria di primo grado. Il fatto che il mondo di oggi è caratterizzato, ora più che mai, da continui e inevitabili incontri tra persone con multiple appartenenze esige un forte impegno volto a favorire pacifici rapporti interculturali. A tale scopo si ritiene che i contenuti dei libri di testo abbiano un ruolo molto rilevante. Di qui, uno degli obiettivi consiste nel verificare se i libri di testo veicolano un’efficace educazione alla conoscenza e al rispetto delle altre culture e religioni, all’ascolto e al dialogo interculturale; nonché al superamento dell'etnocentrismo, degli stereotipi e dei pregiudizi. Si è cercato così di verificare – nel campione dei libri di testo presi in esame – quali eventuali pregiudizi ricorrenti, stereotipi o prospettive etnocentriche vengono costruite, consolidate, reiterate e trasmesse, consapevolmente o inconsapevolmente, attraverso le affermazioni o le immagini che illustrano la cultura arabo-islamica. La prima parte della tesi, quella teorica, è dedicata all'approfondimento di due temi: il primo riguarda il rapporto Oriente-Occidente e la rappresentazione dell'altro e il secondo riguarda invece la condizione della donna musulmana tra stereotipi e realtà. La seconda parte invece, quella empirica, è dedicata principalmente all'analisi del contenuto dei testi di storia. Dall'analisi effettuata è evidente l'interesse, da parte degli autori e degli editori dei libri di testo, per il tema della cultura arabo-islamica. Nonostante ciò, si è potuto riscontrare nei libri presi in esame, sebbene in misura differente, la presenza (o compresenza) di stereotipi, generalizzazioni e informazioni parziali, imprecise o errate attorno alla cultura arabo-islamica e a chi vi appartiene.
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Alexander von Humboldt (1769–1859) was a world traveler, bestselling writer, and versatile researcher, a European salon sensation, and global celebrity. Yet the enormous literary echo he generated has remained largely unexplored. Humboldt inspired generations of authors, from Goethe and Byron to Enzensberger and García Márquez, to reflect on cultural difference, colonial ideology, and the relation between aesthetics and science. This collection of one-hundred texts features tales of adventure, travel reports, novellas, memoirs, letters, poetry, drama, screenplays, and even comics—many for the first time in English. The selection covers the foundational myths and magical realism of Latin America, the intellectual independence of Emerson, Thoreau, Poe, and Whitman in the United States, discourses in Imperial, Weimar, Nazi, East, and West Germany, as well as recent films and fiction. This documented source book addresses scholars in cultural and postcolonial studies as well as readers in history and comparative literature.
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The distribution of denitrification was investigated in the hypolimnion of the east and west lobes of permanently ice-covered Lake Bonney, Taylor Valley, Antarctica. Anomalously high concentrations of dissolved inorganic nitrogen (DIN; nitrate, nitrite, ammonium and nitrous oxide) in the oxygen-depleted hypolimnion of the east lobe of the Lake implied that denitrification is or was active in the west, but not in the east lobe. While previous investigations reported no detectable denitrification in the east lobe, we measured active denitrification in samples from both the east and west lobes. In the west lobe, measured denitrification rates exhibited a maximum at the depth of the chemocline and denitrification was not detectable in either the oxic surface waters or in the deep water where nitrate was absent. In the east lobe, denitrification was detected below the chemocline, at the depths where ammonium, nitrate, nitrite and nitrous oxide are all present at anomalously high levels, Trace metal availability was manipulated in incubation experiments in order to determine whether trace metal toxicity in the east lobe could explain the difference in nitrogen cycling between the 2 lobes. There were no consistent stimulatory effects of metal chelators or nutrient addition on the rate of denitrification in either lobe, so that the mechanisms underlying the unusual N cycle of the east lobe remain unknown. We conclude that all the ingredients necessary to allow denitrification to occur are present in the east lobe. However, even though denitrification could be detected under certain conditions in incubations, denitrification is inhibited under the in situ conditions of the lake.
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Se presenta la primera etapa del relevamiento de los recursos paisajísticos de la provincia de Mendoza, con el ajuste metodológico efectuado mediante una prueba piloto desarrollada sobre la Ruta Nac. N° 7, desde el Acceso sur en Luján de Cuyo (límite este) hasta Potrerillos inclusive (límite oeste). Los límites norte y sur están abarcados por el horizonte observable desde la ruta que atraviesa el área en sentido este-oeste. Se seleccionaron los puntos representativos mediante dos tipos de muestreo: sistemático y discrecional. En base a la catalogación de los recursos visuales se diseña una zonificación referencial general con miras al ordenamiento territorial y uso del suelo en distintas actividades de desarrollo futuro: turístico, reservas, residencial, agrícola, industrial. Se valora la calidad estética del paisaje aplicando, además, índices valorativos de la vulnerabilidad de los espacios a las actividades humanas (Índice de Naturalidad e Índice de Fragilidad), para obtener valores de la Calidad Visual Vulnerable del paisaje. Estos valores se grafican en planos que representan las distintas calidades alcanzadas y se complementa con una descripción de los puntos analizados, recomendaciones para el mejoramiento paisajístico a través de introducción o conducción de vegetación y fotografías documentales de las vistas analizadas.
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In recent sediments of the Stromboli Canyon sides features of mineral and grain size compositions, redox conditions, behavior of Fe, Mn, organic carbon, Mo, and W in an environment of active input of pyroclastic material are considered. Differences in conditions of sedimentation and early diagenesis in the east and west sides of the canyon depending on position of the prevailing direction of drift and steepness of the slopes, as well as types of differentiation of detrital material in sediments under conditions of permanent vibrations are specified.
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Sedimentological and biostratigraphic investigations of 15 cores (total length: 88 m) from the vicinity of Great Meteor seamount (about 30° N, 28° W) showed that the calcareous ooze are asymmetrically distributed around the seamount and vertically differentiated into two intervals. East and west of the seampunt, the upper "A"-interval is characterized by yellowish-brown sediment colors and bioturbation; ash layers and diatoms are restricted to the eastern cores. On both seamount flanks, the sediment of the lower "B"-interval are white and very rich in CaCO3 with a major fine silt (2-16 µ) mode (mainly coccoliths). Lamination, manganese micronodules, Tertiary foraminifera and discoasters, and small limestone and basalt fragments are typical of the "B"-interval of the eastern cores only. The sediments contain abundant displaced material which was reworked from the upper parts of the seamount. The sedimentation around the seamount is strongly influenced by the kind of displaced material and the intensity of its differentiated dispersal: the sedimentation rates are generally higher on the east than on the west flank /e.g. in "B": 0.9 cm/1000 y in the W; 3.1 cm/1000 y in the E), and lower for the "A" than for the "B"-interval. The lamination is explained by the combination of increased sedimentation rates with a strong input of material poor in organic carbon producing a hostile environment for benthic life. The CaCO3 content of the core is highly influenced by the proportion of displaced bigenous carbonate material (mainly coccoliths). The genuine in-situ conditions of the dissolution facies are only reflected by the minimum CaCO3 values of the cores (CCD = about 5,500 m; first bend in dissolution curve = 4,000 m; ACD = about 3,400 m). The preservation of the total foraminiferal association depends on the proportions of in-situ versus displaced specimens. In greater water depths (stronger dissolution), for example, the preservation can be improved by the admixture of relatively well preserved displaced foraminifera. Carbonate cementation and the formation of manganese micronodules are restricted to microenvironments with locally increased organic carbon contents (e.g. pellets; foraminifera). The ash layers consist of redeposited, silicic volcanic glass of trachytic composition and Mio-Pliocene age; possibly, they can be derived from the upper part of the seamount. Siliceous organisms, especially diatoms, are frequent close to the ash layers and probably also redeposited. Their preservation was favoured by the increase of the SiO2 content in the pore water caused by the silicic volcanic glass. The cores were biostraftsraphically subdivided with the aid of planktonic foraminifera and partly alsococcoliths. In most cases, the biostratigraphically determined cold- and warm sections could be correlated from core to core. Almost all cores do not penetrate the Late Pleistocene. All Tertiary fossils are reworked. In general, the warm/cold boundary W2/C2 corresponds with the lithostratigraphic A/B boundray. Benthonic foraminifera indicate the original site deposition of the displaced material (summit plateau or flanks of the seamount). The asymmetric distribution of the sediments around the seamount east and west of the NE-directed antarctic bottom current (AABW) is explained by the distortion of the streamlines by the Coriolis force; by this process the current velocity is increased west of the seamount and decreased east of it. The different proportion of displaced material within the "A" and "B" interval is explained by changes of the intensity of the oceanic circulation. At the time of "B" the flow of the AABW around the seamount was stronger than during "A"; this can be inferred from the presence of characteristic benthonic foraminifera. The increased oceanic circulation implies an enhanced differentiation of the current velocities, and by that, also of the sedimentation rates, and intensifies the winnowed sediment material was transported downslope by turbid layers into the deep-sea, incorporated into the current system of the AABW, and asymmetrically deposited around the seamount.
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O presente trabalho tem como objetivo geral investigar se um grupo de universitários da cidade de São Paulo tem comportamento sexual de risco em relação ao HIV, qual é o conhecimento que o grupo tem sobre HIV/AIDS e quais são as suas dúvidas mais freqüentes sobre o assunto. Além disso, tem como objetivo específico averiguar se o grupo usa a Internet para esclarecer suas dúvidas, quais as estratégias de busca utiliza e se considera que a informação obtida é confiável. Trata-se, portanto, de uma pesquisa exploratória e descritiva, de caráter qualitativo. Como instrumento de campo, construímos um questionário digital de coleta de dados, aplicado pela pesquisadora, usando um computador portátil tipo notebook a 400 estudantes na entrada de quatro unidades de ensino superior da cidade de São Paulo, sendo 100 informantes em cada uma e sendo cada unidade em uma região: Norte, Sul, Leste e Oeste. Além disso, temos ainda o Termo de Consentimento Livre e Esclarecido TCLEconforme determina a Resolução do Conselho Nacional de Saúde CNS 196/96. Para processar e analisar os dados e proceder ao cruzamento das variáveis foram usados procedimentos quantitativos. Para contextualizar nosso objeto, lançou-se um olhar sobre o panorama histórico da Comunicação e Saúde que se articula com a orientação metodológica da pesquisa bibliográfica e documental.
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O presente trabalho tem como objetivo geral investigar se um grupo de universitários da cidade de São Paulo tem comportamento sexual de risco em relação ao HIV, qual é o conhecimento que o grupo tem sobre HIV/AIDS e quais são as suas dúvidas mais freqüentes sobre o assunto. Além disso, tem como objetivo específico averiguar se o grupo usa a Internet para esclarecer suas dúvidas, quais as estratégias de busca utiliza e se considera que a informação obtida é confiável. Trata-se, portanto, de uma pesquisa exploratória e descritiva, de caráter qualitativo. Como instrumento de campo, construímos um questionário digital de coleta de dados, aplicado pela pesquisadora, usando um computador portátil tipo notebook a 400 estudantes na entrada de quatro unidades de ensino superior da cidade de São Paulo, sendo 100 informantes em cada uma e sendo cada unidade em uma região: Norte, Sul, Leste e Oeste. Além disso, temos ainda o Termo de Consentimento Livre e Esclarecido TCLEconforme determina a Resolução do Conselho Nacional de Saúde CNS 196/96. Para processar e analisar os dados e proceder ao cruzamento das variáveis foram usados procedimentos quantitativos. Para contextualizar nosso objeto, lançou-se um olhar sobre o panorama histórico da Comunicação e Saúde que se articula com a orientação metodológica da pesquisa bibliográfica e documental.