987 resultados para Aegean_C-40


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The dynamics of a small linear dune on the northern margin of the Namib Sand Sea have been monitored using erosion pins placed at the dune tip since 1969. GPS measurements of these pins enabled estimation of the rates of advance and lateral migration of the dune. The average rate of advance of the dune tip over the period 1969–2012 was 1.99 m yr–1 towards 015°. Rates of advance and lateral movement varied over the period of monitoring, with a decrease in rates of advance by a factor of 50%, but an increase in the rate of lateral movement. Changes in dune behavior appear to be related to changes in wind regime and the vegetation cover of the interdune area, as a result of increased rainfall in recent years. This study demonstrates the dynamic nature of the tip of this dune and its sensitivity to changes in winds and sand supply.

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At the Paris Peace Conferences of 1918-1919, new states aspiring to be nation-states were created for 60 million people, but at the same time 25 million people found themselves as ethnic minorities. This change of the old order in Europe had a considerable impact on one such group, more than 3 million Bohemian German-speakers, later referred to as Sudeten Germans. After the demise of the Habsburg Empire In 1918, they became part of the new state of Czechoslovakia. In 1938, the Munich Agreement – prelude to the Second World War – integrated them into Hitler’s Reich; in 1945-1946 they were expelled from the reconstituted state of Czechoslovakia. At the centre of this War Child case study are German children from the Northern Bohemian town and district, formerly known as Gablonz an der Neisse, famous for exquisite glass art, now Jablonec nad Nisou in the Czech Republic. After their expulsion they found new homes in the post-war Federal Republic of Germany. In addition, testimonies have been drawn upon of some Czech eyewitnesses from the same area, who provided their perspective from the other side, as it were. It turned out to be an insightful case study of the fate of these communities, previously studied mainly within the context of the national struggle between Germans and Czechs. The inter-disciplinary research methodology adopted here combines history and sociological research to demonstrate the effect of larger political and social developments on human lives, not shying away from addressing sensitive political and historical issues, as far as these are relevant within the context of the study. The expellees started new lives in what became Neugablonz in post-war Bavaria where they successfully re-established the industries they had had to leave behind in 1945-1946. Part 1 of the study sheds light on the complex Czech-German relationship of this important Central European region, addressing issues of democracy, ethnicity, race, nationalism, geopolitics, economics, human geography and ethnography. It also charts the developments leading to the expulsion of the Sudeten Germans from Czechoslovakia after 1945. What is important in this War Child study is how the expellees remember their history while living as children in Sudetenland and later. The testimony data gained indicate that certain stereotypes often repeated within the context of Sudeten issues such as the confrontational nature of inter-ethnic relations are not reflected in the testimonies of the respondents from Gablonz. In Part 2 the War Child Study explores the memories of the former Sudeten war children using sociological research methods. It focuses on how they remember life in their Bohemian homeland and coped with the life-long effects of displacement after their expulsion. The study maps how they turned adversity into success by showing a remarkable degree of resilience and ingenuity in the face of testing circumstances due to the abrupt break in their lives. The thesis examines the reasons for the relatively positive outcome to respondents’ lives and what transferable lessons can be deduced from the results of this study.

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This retrospective study evaluated the epidemiology, treatment and complications of mandibular fracture associated, or not associated, with other facial fractures, when the influence of the surgeon`s skill and preference for ally rigid internal fixation (RIF) system devices was minimized. The files of 700 patients with facial trauma were available, and 126 files were chosen for review. Data were collected regarding gender, age, race, date of trauma, date of surgery, addictions, etiology, signs and symptoms, fracture area, complications, treatment performed, date of hospital discharge.. and medication. 126 patients suffered mandibular fractures associated, or not, with other maxillofacial fractures, and a total of 201 mandibular fractures were found. The incidence of mandibular fractures was more prevalent in males, in Caucasians and during the third decade of life. The most common site was the condyle, followed by the mandibular body. The therapy applied was effective in handling this type of fracture and the Success rates were comparable with other published data.

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A clinical Klebsiella pneumoniae isolate carrying the extended-spectrum beta-lactamase gene variants bla(SHV-40), bla(TEM-116) and bla(GES-7) was recovered. Cefoxitin and ceftazidime activity was most affected by the presence of these genes and an additional resistance to trimethoprim-sulphamethoxazole was observed. The bla(GES-7) gene was found to be inserted into a class 1 integron. These results show the emergence of novel bla(TEM) and bla(SHV) genes in Brazil. Moreover, the presence of class 1 integrons suggests a great potential for dissemination of bla(GES) genes into diverse nosocomial pathogens. Indeed, the bla(GES-7) gene was originally discovered in Enterobacter cloacae in Greece and, to our knowledge, has not been reported elsewhere.

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The Central Atlantic Magmatic Province (CAMP), emplaced at the Triassic-Jurassic (T-J) boundary (-200 Ma), is among the largest igneous provinces on Earth. The Maranhao basin in NE Brazil is located around 700 km inland and 2000 km from the site of the earliest Pangea disruption. The CAMP tholeiites occur only in the western part of the basin and have been described as low and high-Ti. Here we document the occurrence of two sub-groups among the high-Ti tholeiites in the Western Maranhao basin. The major and trace elements and the Sr-Nd-Pb isotopic ratios define three chemical groups corresponding to the low-Ti (TiO(2)< 1.3 wt.%), high-Ti (TiO(2)-2.0 wt.%) and evolved high-Ti (TiO(2 >)3 wt.%) western Maranhao basin tholeiites (WMBT). The new (40)Ar/(39)Ar plateau ages obtained on plagioclase separates for high-Ti (199.7 +/- 2.4 Ma) and evolved high-Ti WMBT (197.2 +/- 0.5 Ma and 198.2 +/- 0.6 Ma) are indistinguishable and identical to those of previously analyzed low-Ti WMBT (198.5 +/- 0.8 Ma) and to the mean (40)Ar/(39)Ar age of the CAMP (199 +/- 2.4 Ma). We also present the first Re-Os isotopic data for CAMP basalts. The low and high-Ti samples display mantle-like initial ((187)Os/(188)Os)(i) ranging from 0.1267 to 0.1299, while the evolved high-Ti samples are more radiogenic (((187)Os/ (188)Os)(i) up to 0.184) We propose that the high-Ti WMBT were derived from the sub-lithospheric asthenosphere, and contaminated during ascent by interaction with the subcontinental lithospheric mantle (SCLM). The evolved high-Ti WMBT were derived from the same asthenospheric source but experienced crustal contamination. The chemical characteristics of the low-Ti group can be explained by partial melting of the most fertile portions of the SCLM metasomatized during paleo-subduction. Alternatively, the low-Ti WMBT could be derived from the sub-lithospheric asthenosphere but the resulting melts may have undergone contamination by the SCLM. The occurrences of high-Ti basalts are apparently not restricted to the area of initial continental disruption which may bring into question previous interpretations such as those relating high-Ti CAMP magmatism to the initiation of Atlantic ridge spreading or as the expression of a deep mantle plume. We propose that the CAMP magmatism in the Maranhao basin may be attributed to local hotter mantle conditions due to the combined effects of edge-driven convection and large-scale mantle warming under the Pangea supercontinent. The involvement of a mantle-plume with asthenosphere-like isotopic characteristics cannot be ruled out either as one of the main source components of the WMBT or as a heat supplier. (C) 2010 Elsevier BM. All rights reserved.

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New U-Pb zircon and (40)Ar-(39)Ar K-feldspar data are presented for syn-sedimentary volcanogenic rocks from the Neoproterozoic Marica Formation, located in the southern Brazilian shield. Seven (of nine) U-Pb sensitive high-resolution ion microprobe analyses of zircons from pyroclastic cobbles yield an age of 630.2 +/- 3.4 Ma (2 sigma), interpreted as the age of syn-sedimentary volcanism, and thus of the deposition itself. This result indicates that the Marica Formation was deposited during the main collisional phase (640-620 Ma) of the Brasiliano II orogenic system, probably as a forebulge or back-bulge, craton-derived foreland succession. Thus, this unit is possibly correlative of younger portions of the Porongos, Brusque, Passo Feio, Abapa (Itaiacoca) and Lavalleja (Fuente del Puma) metamorphic complexes. Well-defined, step-heating (40)Ar-(39)Ar K-feldspar plateau ages obtained from volcanogenic beds and pyroclastic cobbles of the lower and upper successions of the Marica Formation yielded 507.3 +/- 1.8 Ma and 506.7 +/- 1.4 Ma (2 sigma), respectively. These data are interpreted to reflect total isotopic resetting during deep burial and thermal effects related to magmatic events. Late Middle Cambrian cooling below ca. 200 degrees C, probably related to uplift, is tentatively associated with intraplate effects of the Rio Doce and/or Pampean orogenies (Brasiliano III system). In the southern Brazilian shield, these intraplate stresses are possibly related to the dominantly extensional opening of a rift or a pull-apart basin, where sedimentary rocks of the Camaqua Group (Santa Barbara and Guaritas Formations) accumulated.

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Börsnoterade bolag ska i sin koncernredovisning redovisa enligt IFRS och förvaltningsfastigheter skall redovisas enligt IAS 40 Förvaltningsfastigheter. Detta examensarbete undersöker hur Nordiska börsnoterade bolag tillämpar vissa punkter inom IAS 40 i 2014 års redovisning jämfört med 2009 års redovisning. Syftet med undersökningen är att undersöka skillnader mellan de granskade företagens redovisning 2014 och 2009, med utgångspunkten i en tidigare publicerad undersökning (Hedlund & Ersson, 2011). Det som undersöks är om företagen använder samma värderingsmetod, om de informerar om hur värdering av förvaltningsfastigheter skett, om var i resultatrapporten de rapporterar justeringar av verkligt värde samt hur väl de lämnar upplysningar enligt IAS 40 punkt 75. Undersökningen har skett med en kvantitativ metod då det är årsredovisningar som granskats. Undersökt data är årsredovisningar från 2014 och 2009 för samma företag som granskats i den tidigare undersökningen. Några företag har utgått då de inte ingår i urvalsramen Nordiskt börsnoterat fastighetsbolag. Totalt granskades 14 stycken företag. Resultatet visar att efterlevnaden totalt sett är något bättre 2014 jämfört med den tidigare undersökningen. Till stor del beror det på urvalet där de företag som utgått var dåliga på att lämna upplysningar enligt IAS 40 i 2009 års redovisning. Sett till de företag som är med i båda undersökningarna är efterlevnaden likartad de jämförda åren. Det är få företag som lämnar upplysningar om begränsningar i rätten att sälja förvaltningsfastigheter, avtalsenliga förpliktelser att köpa eller hur de skiljer på rörelsefastigheter och förvaltningsfastigheter. Tolkningen kan då göras att det inte finns någon restriktion eller förpliktelse om det inte lämnas några sådana upplysningar. Om det är ett fastighetsbolag så kan det tolkas som att de inte har några rörelsefastigheter. Med dessa tolkningar blir efterlevnaden bland de undersökta företagen god.

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Now 40, Colby’s Environmental Studies Program is growing exponentially, equipping students to tackle real-world problems.

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Legendary coach Dick Whitmore retires after 40 years, but his relationship with his “basketball people” endures.

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Esta dissertação tem como objetivo principal identificar dados e elaborar um estudo sobre a produção arquitetônica da cidade de Pelotas de 1758 ao fim da década de 40 do século XX, analisando as características peculiares de tal produção e as transformações decorrentes do abandono dos padrões historicistas e da implantação de uma arquitetura moderna. Nesse sentido, traduz-se em revisão de parte da própria história da cidade, da qual a arquitetura é manifestação e testemunho significativo.

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O objetivo deste trabalho foi avaliar a atividade proliferativa das células epiteliais da mucosa lingual de camundongos frente à ação do etanol a 40° GL, baseado na contagem e mensuração das áreas das AgNORs através da técnica de impregnação pela prata. Foram utilizados 32 camundongos com 2 meses de vida, divididos em três grupos. Os grupos controle e aplicação tópica receberam ração padrão e água comum, sendo o último submetido ainda a 2 aplicações tópicas semanais de 1ml de etanol a 40 °GL. No grupo ingestão a água foi substituída por etanol na mesma graduação alcoólica. Os animais foram biopsiados no centro do dorso da língua, no início, aos 6 e 12 meses de experimento, e as peças submetidas ao processamento de rotina para inclusão em parafina. Fizeram-se cortes histológicos de 4 µm submetidos à técnica de impregnação pela prata. Foram avaliadas a contagem e área das AgNORs de 50 células da camada basal e 50 da camada suprabasal. Os resultados foram comparados pelo teste da análise da variância (ANOVA) e teste post-hoc da mínima diferença significativa (LSD). Observou-se um aumento da média do número e da área das AgNORs na camada suprabasal aos 12 meses, no grupo ingestão (p < 0,05). Conclui-se que a ingestão de etanol a 40° GL provoca um aumento da proliferação celular na mucosa bucal.