Novos territórios da escritura: reflexões sobre exotismo e identidade em Amélie Nothomb e Adriana Lisboa

O exotismo, em sua projeção literária, é um conceito relacionado ao imperialismo e ao relato da aventura. Cabe, assim, questionar o emprego de semelhante conceito na produção literária contemporânea, inserida em um mundo mapeado, cosmopolita e de fronteiras fluidas. No esteio da reflexão sobre o exotismo literário no século XXI, os conceitos de alteridade e de identidade ganham peso, expondo um sujeito multifacetado e descentrado, que se equilibra na corda bamba entre realidade e ficção. Está preparado, assim, o terreno para a transgressão de gêneros canônicos, como a autobiografia, gerando novas perspectivas de abordagem do posicionamento do autor no campo literário e ampliando conceitos como os de autoficção e de espaço biográfico. No mesmo movimento, o fenômeno da desterritorialização conduz autores e leitores a novos espaços, nem sempre físicos, mas talvez propícios a inéditas viagens pelo caminho da arte

O sistema fluvio-estuarino da Baía de Sepetiba preservado na estratigrafia rasa da plataforma continental interna adjacente (RJ)

A análise de dados de reflexão sísmica monocanal boomer (Hz ~ 700-4,000; penetração ~ 70 ms) adquiridos na plataforma continental interna-média (até ~ 50-60 m de profundidade) ao largo do sistema estuarino baía de Sepetiba, no Estado do Rio de Janeiro, Brasil, revelou a ocorrência de uma sucessão sedimentar preservada 15-20 m, sismicamente interpretada como representando ambientes fluvio-estuarinos para marinhos rasos. Estas séries são sotopostas à inconformidade regional mais superior reconhecida na escala de plataforma, chamada superfície S3. Esta superfície é erodida por numerosas incisões fluviais, que sugerem processos erosivos associados à prolongada exposição subaérea da plataforma continental durante o estágio isotópico marinho 2 (MIS 2), globalmente datada em ~ 20 ka A.P.. A preservação de tais unidades de corte e preenchimento estuarinho presumíveis Pleistoceno Superior-Holoceno na plataforma interna-média (até ~ 30 km da costa) evidencia pela primeira vez na área a existência de um paleo sistema fluvial bastante desenvolvido e processos dominantes de denudação na bacia hidrográfica a montante que atualmente alimenta a baía de Sepetiba. Bem como que, uma série de elementos arquiteturais sísmicos dentro desta sucessão estuarina, como canais de maré retrogradantes, registram a evolução do paleo sistema estuarino de um sistema aberto à um sistema parcialmente protegido durante a transgressão Holocênica. A formação e erosão de uma sucessão de ilhas barreira isoladas e canais de maré durante a transgressão persistiu até o desenvolvimento de uma superfície estratigráfica superior na área, interpretada como a superfície de máxima inundação (MFS) no registro estratigráfico. A ilha barreira atual (restinga da Marambaia) prograda sobre a MFS como uma feição deposição regressiva, apontando para uma idade mais jovem do que cerca de ~ 5 ka A. P., idade da transgressão máxima na área, de acordo com a literatura disponível.

A influência da habilidade empática sobre o perdão interpessoal

Diversos estudos têm apontado os benefícios da habilidade empática. Ela está associada à saúde e bem-estar psicológicos, a relacionamentos mais satisfatórios, a comportamentos pró-sociais e morais, à resiliência etc., ao passo que sua ausência está associada a diversos prejuízos pessoais e interpessoais. Como habilidade social, entende-se que a empatia é um fenômeno multidimensional, com aspectos cognitivos, afetivos e comportamentais. Respectivamente, envolve a capacidade de compreender o ponto de vista do outro, de se interessar genuinamente pelo seu bem-estar, e de expressar, por meio de comportamentos verbais e/ou não verbais, sua compreensão e interesse ao interlocutor, permitindo a este se sentir entendido e validado em suas experiências. Esta habilidade tem sido associada, mais recentemente, por diversos estudos internacionais, à capacidade de perdoar um ofensor por suas transgressões. Com isso, o propósito do presente trabalho foi investigar a influência da habilidade empática sobre o perdão interpessoal, em uma amostra brasileira. O perdão também vem sendo considerado uma experiência multifatorial, com domínios cognitivos, afetivos e comportamentais, que abrangem os pensamentos, as emoções e os comportamentos em relação a um ofensor. Para a realização desta investigação, 172 participantes responderam o Inventário de Empatia (IE), a Escala de Atitudes (o Enright Forgiveness Inventory EFI) e uma ficha sobre dados socidemográficos. O IE apresenta quatro subescalas: Tomada de Perspectiva, Sensibilidade Afetiva, Flexibilidade Interpessoal e Altruísmo. O EFI apresenta uma Escala Global de perdão e três Subescalas: Afetiva, Cognitiva e Comportamental. Testes correlacionais e de regressão foram processados a fim de investigar as relações entre os fatores do IE e do EFI, bem como a predição da empatia sobre o perdão. Os resultados indicaram diversas relações positivas e significativas estatisticamente: a Tomada de Perspectiva se relacionou à Escala Global do perdão e às Subescalas Afetiva e Comportamental; a Sensibilidade Afetiva e o Altruísmo se relacionaram à Escala Global e à Comportamental do perdão; a Flexibilidade Interpessoal foi o único fator empático que não apresentou correlações significativas com o perdão. Com a regressão, constatou-se que: Altruísmo e Tomada de Perspectiva, combinados, ou Tomada de Perspectiva, sozinha, predisseram o Perdão Global; Sensibilidade Afetiva, Tomada de Perspectiva e Altruísmo, combinados ou individualmente, tiveram valor preditivo sobre a Subescala Comportamental do perdão; e apenas a Tomada de Perspectiva, sozinha, predisse a Subescala Afetiva do perdão. Nenhum fator do IE teve valor preditivo sobre a Subescala Cognitiva do perdão e a Flexibilidade Interpessoal não predisse qualquer dimensão do EFI. Os resultados encontrados apoiam pesquisas anteriores, confirmando a importância da empatia para a ocorrência do perdão interpessoal. Contudo, ressalta-se que a Tomada de Perspectiva se destacou como a dimensão empática mais importante, sugerindo a relevância que a capacidade de adotar o ponto de vista do outro tem para que o perdão seja alcançado.

Ética para além da moral: os apelos para o reconhecimento na escola

Este trabalho tem como proposta problematizar os atos de transgressões operados no cotidiano escolar sob os preceitos da ética e dos valores morais. Na interseção entre filosofia, psicanálise e educação tecemos nossa reflexão sobre o assunto, deflagrando alguns estudos pertinentes aos discursos conceituais, à questão da constituição dos sujeitos e das regras sociais, bem como de um fazer docente que questione os atos de transgressão no espaço da educação. Tal pesquisa se deve à inquietação provocada pelo contexto da sociedade hodierna, a qual, mergulhada numa grave crise de violência e de valores éticos, reavalia e revalida princípios e conceitos que, nitidamente, diante de uma conjuntura cada vez mais inclinada aos apelos do capital, vem deixando de nortear as relações sociais no decorrer dos anos. Neste contexto, o docente é cada vez mais convocado a desempenhar papéis que outrora pertenciam a outras categorias sociais, principalmente, com o avanço das escolas públicas de tempo integral. Aludimos assim a esta realidade, o desafio de engajar a ação educativa em demandas de eticidade. Aparar as arestas de um objeto de investigação tão amplo não é tarefa simples, portanto, consideraremos alguns recortes da constituição psíquica e social dos sujeitos. Analisando o lugar da ética na relação ensino/aprendizagem, no processo de formação escolar e no fazer docente, trabalhamos com o pressuposto de que a tensão sofrida cotidianamente pela criança e pelo adolescente, de um lado pelo tecido social, família, escola e Estado e do outro, pelo desejo de ser reconhecido nos grupos sociais, podem mesmo acirrar comportamentos inadequados e violentos na escola. Portanto, a postura adotada pelo educador frente aos conflitos internos e externos do aluno poderá, paradoxalmente, facilitar ou mesmo impedir uma dada má ação no seio da escola. Nossa finalidade é promover reflexões possíveis sobre as dimensões da ética nas relações manifestadas principalmente entre o docente e o aluno, acreditando que a existência de um espaço coletivo de discussão poderá contribuir para que ambos encontrem saídas próprias frente aos impasses que a questão ético/moral no âmbito educativo impõe.

Arte como religião: pensando a busca religiosa através de separações

Arte como Religião é um convite à reflexão sobre religião por meio de trabalhos artísticos. A pesquisa artística, poética e filosófica sobre a relação fronteiriça entre arte e religião teve seu ponto de partida na minha história pessoal e foi desenvolvida relacionando as ideias de separação e alteridade como essenciais para a religião, e as ideias de transgressão e linguagem como essenciais para a observação da arte. O conceito poético foi delimitado pelos trabalhos artísticos Relicários de Santos Vivos e Canonizador AcSeita Coletivo, que partindo da ideia da separação busca isolar a figura dos santos como os seres autorizados à busca religiosa e à prática de lidar com o sagrado, passando-se a observar, por meio dos objetos utilizados pelos mesmos, as mudanças de valores sociais

Foraminíferos como indicadores paleoecológicos do Holoceno no Manguezal de Guaratiba, Baía de Sepetiba, Rio de Janeiro

Os manguezais são ecossistemas estuarinos, representando a transição entre os ambientes continentais e marinhos, e tendo sua formação relacionada com as flutuações do nível do mar no Quaternário. No Manguezal de Guaratiba, diversos estudos sobre as variações do nível do mar, mais precisamente no Holoceno, têm sido realizados, sob os enfoques sedimentológicos, geoquímicos, palinológicos e micropaleontológicos. Entre os estudos micropaleontológicos, destacam-se os que utilizam os foraminíferos bentônicos, micro-organismos amplamente utilizados como indicadores paleoecológicos e paleoambientais do Holoceno. No presente trabalho, foi coletado, através de um amostrador do tipo trado russo, um testemunho (T1) no Manguezal de Guaratiba, no qual foram realizadas análises de parâmetros como granulometria, teores de matéria orgânica (MO), carbonato, carbono orgânico total (COT) e enxofre (S) (abióticos) e da fauna de foraminíferos bentônicos (bióticos). Foram utilizadas também índices ecológicos e análises de agrupamento, através das quais foi possível estabelecer quatro associações faunísticas (I,II,III e IV), assim como os fatores ambientais que mais influenciaram a distribuição da fauna. A correlação com assembleias de foraminíferos de outros testemunhos que possuem datação por Carbono 14 (C14), assim como outros trabalhos que versam sobre a evolução da Baía de Sepetiba, permitiu o estabelecimento de três ciclos de emersão-submersão para a área da planície de maré estudada: 1)Fase transgressiva: nível de concentração de conchas em depósitos lagunares formados por sedimentos finos, sem foraminíferos; provavelmente posterior a uma regressão; 2) Fase transgressiva: formação de uma baía, com presença exclusiva de espécies de foraminíferos calcários (Associação III) com maiores valores de riqueza e queda nos valores de COT; ocorrida há cerca de 3.800 anos A.P 3) Fase transgressiva: período de submersão, presença de espécies de foraminíferos tipicamente estuarinos (Associação IV), com duração entre 3.500 anos A.P. e 2.700 anos A.P.; 4)Fase transgressiva: caracterizada pela alternância entre a formação de baías rasas e lagunas marinhas (maiores índices de riqueza nas associações faunísticas), menores valores de MO e COT e aumento na proporção de sedimentos finos; evento iniciado há cerca de 2.700 anos A.P.; e 5)Fase regressiva: fauna de foraminíferos aglutinantes, resistente às condições de salinidade e acidez características de ambientes confinados como os manguezais, além do incremento nos teores de areia, evidenciando a fase final de confinamento da Baía de Sepetiba pela Restinga da Marambaia; evento iniciado por volta de 2.400 anos A.P., estendendo-se até o presente. Os resultados obtidos mostram a importância da correlação lateral entre testemunhos na interpretação paleoambiental da Baía de Sepetiba, além da identificação de estágios de transgressão e regressão que se aproximam da curva de variação do nível do mar proposta por SUGUIO et al.(1985) para o litoral do Estado do Rio de Janeiro

Coherence between solar activity and the East Asian winter monsoon variability in the past 8000 years from Yangtze River-derived mud in the East China Sea

AMS(14)C dating and grain-size analysis for Core PC-6, located in the middle of a mud area on the inner shelf of the East China Sea (ECS), were used to rebuild the Holocene history of the East Asian winter monsoon (EAWM). The 7.5-m core recorded the history of environmental changes during the postglacial transgression. The core's mud section (the upper 450 cm) has been formed mainly by suspended sediment delivered from the Yangtze River mouth by the ECS Winter Coastal Current (ECSWCC) since 7.6 kyr BP. Using a mathematical method called "grain size vs. standard deviatioW', we can divide the Core PC-6's grain-size distribution into two populations at about 28 mu m. The fine population (< 28 mu m) is considered to be transported by the ECSWCC as suspended loads. Content of the fine population changes little and represents a stable sedimentary environment in accord with the present situation. Thus, variation of mean grain-size from the fine population would reflect the strength of ECSWCC, which is mainly controlled by the East Asian winter monsoon. Abrupt increasing mean grain size in the mud section is inferred to be transported by sudden strengthened ECSWCC, which was caused by the strengthened EAWM. Thus, the high resolution mean grain-size variation might serve as a proxy for reconstruction of the EAWM. A good correlation between sunspot change and the mean grain-size of suspended fine population suggests that one of the primary controls on centennial- to decadal-scale changes of the EAWM in the past 8 ka is the variations of sun irradiance, i.e., the EAWM will increase in intensity when the number of sunspots decreases. Spectral analyses of the mean grain-size time series of Core PC-6 show statistically significant periodicities centering on 2463, 1368, 128, 106, 100, 88-91, 7678, and 70-72 years. The EAWM and the East Asian summer monsoon (EASM) agree with each other well on these cycles, and the East Asian Monsoon (EAM) and the Indian Monsoon also share in concurrent cycles in Holocene, which are in accord with the changes of the sun irradiance. (c) 2005 Elsevier B.V. All rights reserved.

准噶尔盆地滴南凸起中生界层序地层及有利勘探目标优选

Based on the theories of sequence stratigraphy and sedimentology, as well as comprehensive studies of seismic data, drilling data, core interpretation and setting of this area, the thesis presents an analysis for Mesozoic formation in Dinan uplift. By means of recognizing the boundary of the sequence, dividing and correlating the systems tract, Mesozoic of Dinan uplift is divided into ten sequences and twenty-five systems tracts during the establishment of the sequence framework. In the framework, some sequences are featured by mature systems of lowstand, water-transgression and highstand, while some undeveloped systems of lowstand or highstand. The main sedimentary facies in Mesozoic of Dinan uplift are braided river, meandering river, delta and lake. The braided river was divided into sandy river and rudaceous river by the lithology of the river channel and was divided into dry climate and wet climate condition by the color of the flood plain. Additionally, The concept of “wetland” is put forward for the first time and regarded as the consequence of wet climate. The analysis includes the classification of six types of traps: (1) stratigraphic overlap trap, (2) lithologic trap with updip pinchout, (3) stratigraphic unconformity trap, (4) fault-lithology trap, (5) fault trap, (6) anticlinal trap, and combining with the research of the characteristics and distribution rules for the known reservoir, it draws out that “fault control” is the petroleum accumulation pattern in this area, in which fault is the key element of the transporting system. Finally the thesis concludes the distribution characteristics and optimized some targets for the potential exploration zone.

新元古代陡山沱期古海洋的氧化还原环境演变

High resolution geochemical analysis of Ediacaran Doushantuo Formation deposits in eastern Gorges area, including carbon and sulfur isotope compositions, trace elements, rare earth elements, and so on, show a whole panorama of the oceanic environment in Ediacaran Doushantuo Formation. The deposits of Doushantuo II recorded consistent δ13Corg values and variable δ13Ccarb values, which suggets that it is strongly redox stratified in Doushantuo ocean, and there is a large DOC reservior in the deep ocean. The redox state of Doushantuo ocean in Yangtze area was not steady. The movement of chemocline was concerned with the transgression and/or regression. During the transgression, raising sea level and upwelling with anoxic deep water would cause the ocean anoxic; during the regression, declining sea level and weathered sulfate input would cause the suface ocean becoming oxic. The oxidations of this DOC reservior would caused negative δ13C excurions in Doushantuo Formation. Comparing with oceanic redox states and fossils productivity, we found that the stratum with high biologic productivity and diversity did not indicated oxic conditions. In the opposite, these stratum recorded anoxic conditions. We suggeste that it would be relatived to burial and preservation of fossils, because anoxic conditions are in favor of burial and preservation of fossils. It is proved that methane seep occurred at the base of Duoshantuo cap carbonate. However, comparing cap carbonate with seep carbonate, we found that oxidation of methan and the post-diagenesis could not derictely result in cap carbonate deoposition. Cap carbonate would be derived from the high level CO2 in atomosphere.

黄东海及朝鲜海峡冰后期陆架沉积物的环境磁学研究

There are four chapters in this dissertation. The first chapter briefly synthesizes the basic theories, methods and present-day applying situation of environmental magnetism. The second chapter probes into the magnetic mineral diagenesis in the post-glacial muddy sediments from the southeastern South Yellow Sea and its response to marine environmental changes, using the muddy sediment of Core YSDP103 formed in the shelf since about 13 ka BP. The third chapter illustrates the high-resolution early diagenetic processes by investigating the rapidly deposited muddy sediments during the last 6 ka in Cores SSDP-102 and SSDP-103 from the near-shore shelf of Korea Strait. The fourth chapter presents the results of detailed rock magnetic investigation of the surface sediments from the fine-grained depositional area on the outer shelf of the East China Sea in an attempt to provide environmental magnetic evidence for the provenance of the fine-grained deposit. Core YSDP103 was retrieved in the muddy deposit under the cold eddy of the southeastern South Yellow Sea, and the uppermost 29.79 m core represents the muddy sediments formed in the shelf since about 13 ka BP. The lower part from 29.79 to 13.35 m, called Unit A2, was deposited during the period from the post-glacial transgression to the middle Holocene (at about 6 ~(14)C ka BP) when the rising sea level reached its maximum, while the upper part above 13.35 m (called Unit Al) was deposited in a cold eddy associated with the formation of the Yellow Sea Warm Current just after the peak of post-glacial sea level rise. For the the uppermost 29.79 m core, detailed investigation of rock-magnetic properties and analyses of grain sizes and geochemistry were made. The experimental results indicate that the magnetic mineralogy of the core is dominated by magnetite, maghemite and hematite and that, except for the uppermost 2.35 m, the magnetic minerals were subject to reductive diagenesis leading to significant decline of magnetic mineral content and the proportion of low-coercivity component. More importantly, ferrimagnetic iron sulphide (greigite) is found in Unit A2 but absent in Unit Al, suggesting the control of marine environmental conditions on the magnetic mineral diagenesis. Magnetic parameters show abrupt changes across the boundary between the Unit Al and A2, which reflects a co-effect of environmental conditions and primary magnetic components of the sediments on the diagenesis. Alternating zones of high and low magnetic parameters are observed in Unit A2 of Core YSDP103, which is presumably due to periodic changes of the concentration and/or grain size of magnetic minerals carried into the study area. Cores SSDP-102 and SSDP-103, two studied sediment cores from the Korea Strait contain mud sequences (14 m and 32.62 m in thickness) that were deposited during the last 6,000 years. Analyses of grain sizes and geochemistry of the cores have demonstrated that the sediments have uniform lithology and geochemical properties, however, marked down-core changes in magnetic properties suggest that diagenesis has significantly impacted the magnetic properties. An expanded view of early diagenetic reactions that affect magnetic mineral assemblages is evident in these rapidly deposited continental shelf sediments compared to deep-sea sediments. The studied sediments can be divided into four descending intervals, based on magnetic property variations. Interval 1 is least affected by diagenesis and has the highest concentrations of detrital magnetite and hematite, and the lowest solid-phase sulfur contents. Interval 2 is characterized by the presence of paramagnetic pyrite and sharply decreasing magnetite and hematite concentrations, which suggest active reductive dissolution of detrital magnetic minerals, the absolute minimum abundance of magnetite is reached at the end of this interval. Interval 3 is marked by a progressive loss of hematite with depth, and at the base of this interval, 82% to 88% of the hematite component was depleted and the bulk magnetic mineral concentration was reduced to the lowest value in the entire studied mud section. Interval 4 has an increasing down-core enhancement of authigenic greigite, which is interpreted to have formed due to arrested pyritization resulting from consumption of pore water sulfate with depth. This is the first clear demonstration from an active depositional environment for a delay of thousands of years for acquisition of a magnetization carried by greigite. This detailed view of diagenetic processes in continental shelf sediments suggests that studies of geomagnetic field behavior from such sediments should be conducted with care. Paleoceanographic and paleoclimatic studies based on the magnetic properties of shelf sediments with high sedimentation rates like those in the Korea Strait are also unlikely to provide a meaningful signature associated with syn-depositional environmental processes. The rock magnetic properties of the surface sediments from the fine-grained depositional area on the outer shelf of the East China Sea, an area surrounded by sands, are investigated with a view to providing information on the sediment provenance. Multiple magnetic parameters such as magnetic susceptibility (%), anhysteretic remanent magnetization (ARM), saturation rernanent magnetization (SIRM), coercivities of SIRM (Her), and S ratios (relative abundance of low-coercivity magnetic minerals) are measured for all 179 surface samples, and partial representative samples are examined for their magnetic hysteresis parameters, temperature-dependence of magnetic susceptibility and x-ray diffraction spectra. Our research indicates that the magnetic mineralogy is dominated by magnetite with a small amount of hematite and is primarily of pseudo-single domain (PSD) to multidomain (MD) nature with a detrital origin. In the surface sediments, the granulometry of magnetic fractions is basically independent of grain sizes of the sediment containing the magnetic grains, and the composition of magnetic minerals remains almost homogeneous, that is, with a relatively constant ratio of low to high coercivity fraction throughout the area. The magnetic concentration in the study area generally decreases to the east or southeast accompanied by magnetic-particle fining to the east or to the northeast. The geographic pattern of magnetic properties is most reasonably explained by a major source of sediment jointly from the erosion of the old Huanghe River deposit and the discharge of the Changjiang River. The rock magnetic data facilitate understanding of the transport mechanism of fine-grained sediments in the outer shelf of the East China Sea.

东营凹陷沙三中亚段湖相浊积岩储层特征及油气成藏规律研究

Turbidity sandstone reservoirs have been an important field of hydrocarbon exploration and development in the basins all over the world, as well as in China. Lithologic pools are composed of turbidity sandstones and other sandstones are frequently found in the Jiyang Depression that is a Mesozoic-Cenozoic non-marine oil-bearing basin. The Dongying Sag lies in the sedimentary center of the basin. The subtle traps with turbidity reservoirs are generally difficult to be predicted and described by using current techniques. The studies on turbidity reservoirs plays thus an important theoretical and theoretical practical role in exploration and development in the Jiyang Depression. The attention is, in this thesis, focused on the petrologic properties and oil accumulating behaviors in lake turbidity sedimentary systems in the middle part of the third section of Shahejie Formation in the Dongying Sag, especially in Dongxin area, which lies on the central uplift of the Sag. The paper has disclosed the origin types of turbidity sandstones, distribution pattern and controlling factors of turbidity sandstones, and set up hydrocarbon accumulation patterns of the middle part of the third section of Shahejie Formation in Dongxin, based on nonmarine high resolution sequence stratigraphy, event sedimentology and new theories of hydrocarbon forming. By studying prediction method and technology of turbidity sandstone reservoirs, using precise geological model developing, new techniques of high resolution seismic inversion constrained by logging, the paper has forecast low permeability turbidity sandstone reservoirs and pointed out advantage exploration aims to progressive exploration and development. The paper has obtained mainly many productions and acknowledges as follows: 1.Turbidity sandstone reservoirs of the third section of Shahejie Formationin Dongying Sag are formed in such specifical geological background as rift and extension of basin. The inherited Dongying delta and transgression make up many turbidity distribution areas by overlaying and joining together. The hydrocarbon migrates from depression area to adjacent turbidity sandstone continuously. Accumulation area which is sufficient in oil is formed. 2.The paper has confirmed distinguishable sign of sequence boundary , established stratigraphic framework of Dongying Sag and realized isotime stratigraphic correlation. Es3 of Dongying delta is divided into eleven stages. Among them, the second period of the lower section in Es3, the sixth period of the middle section in Es3, the third period of the upper section in Es3 correspond to eleven sedimentary isotime surface in seismic profile, namely Es3 is classified into eleven Formations. 3.According to such the features of turbidity sandstone as deep in burial, small in area, strong in subtle property, overlaying and joining together and occurring in groups, management through fault and space variations of restriction quantum are realized and the forecast precision of turbidity sandstone by using precise geological model developing, new techniques of high resolution seismic inversion constrained by logging, based on the analysis of all kinds of interwell seismic inversion techniques. 4.According to the features of low permeable turbidity sandstone reservoirs, new method of log interpretation model is put forward. At the same time, distinguish technology of familiar low resistivity oil layer in the turbidity sandstone reservoirs is studied based on petrophysical laboratory work and "four properties" interrelationship between lithological physical Jogging and bearing hydrocarbon properties. Log interpretation model and reservoir index interpretation model of low resistivity oil layer are set up. So the log interpretation precision is improved. 5.The evolution law and its difference of the turbidity sandstone are embodies as follows: the source of sediments come from the south and east of the study area in the middle period of Es3. East source of sediments is pushed from west to east. However, the south source supply of sediments in the early and middle period of Es3 is in full, especially in Es3. subsequently, the supply is decreased gradually. Turbidity fan moves back toward the south and the size of fan is minished accordingly. The characteristic of turbidity sandstone in Dongying Sag is different in different structural positions. Dongxin in the middle-east of the central lift and Niuzhuang Sag He in Dongying delta front and prodelta deep lake subfacies. Although the turbidity sandstone of the two areas root in the Dongying delta sedimentary system, the sand body has different remarkably characteristic. 6.The sedimentary model of the turbiditys in study area have three types as follows: (1) collapse turbidity fan in respect of delta; (2) fault trench turbidity fan; (3) other types of microturbidity sandstone. Middle fan and outer fan, can be found mainly in sublacustrine fan. Middle fan includes braided channel microfacies, central microfacies and braided interchannel microfacies, which is main prospecting oil-bearing subfacies. The middle section of the third section of Shahejie Formation in study area (for example the central lift) can be divided into middle-lower and upper part. The middle-lower part is characteristic of turbidity fan. The upper part is sedimented mainly by delta-collapse fan. 7.The turbidity reservoirs of the middle part of the third section of Shahejie Formation in study area characterize by low maturity both in component and texture, strong in diagenesis and low in permeability. The reservoir can be classified into four types. Type III is the body of reservoir and comprises two types of H a and HI b. M a belongs to middle porosity - low permeability reservoir and distributes in the central lift. Hlb belongs to low porosity - low permeability and distributes in Haojia region. 8.A11 single sand body of lens turbidity reservoir of the middle part of the third section of Shahejie Formation in study area are surrounded by thick dark source rocks. The oil-water system is complex and behaves that every sandstone is single seal unit. The water body is 1/3-1-5 of the sand body. The edge water is not active. The gas exists in the top of reservoir in the form of mixed gas. For far-range turbidity fan with big scale channel, the area and volume of sand body is large and the gap is big in oil packing degree. There are lots of edge water and bottom water, and the latter increases rapidly during the course of development. 9.By exerting the modern hydrocarbon forming theories, the third section of Shahejie Formation in study area belongs to abnormally pressured fluid compartment. The lithological reservoir of the third section of Shahejie Formation is formed in the compartment. The reservoir-formed dynamic system belongs to lower self-source enclosed type. The result and the practice indicate that the form and accumulation of lithological oil reservoirs are controlled by the temperature and pressure of stratum, microfacies, thickness of sand body, fault and reservoir heterogeneity. 10. Based on studies above, the emphases focus on in south and north part of Dongying structure, west Dongxin region and south part Xinzhen structure in the application of production. The practice proves that the turbidity sandstone reservoirs in Ying 11 block and the fault-lithological reservoirs in Xin 133 block have been obtained significant breakthrough. The next target is still sandstone groups of the third section of Shahejie Formation in the bordering areas of Dongxin region for instance Xin 149 area, He 89 area, Ying 8 area etc.

James Joyce and the Problem of Psychoanalysis

Thurston, L. (2004). James Joyce and the Problem of Psychoanalysis. Cambridge: Cambridge University Press. RAE2008

Reliability of antitransglutaminase antibodies as predictors of gluten-free diet compliance in adult celiac disease.

OBJECTIVE: Strict lifelong compliance to a gluten-free diet (GFD) minimizes the long-term risk of mortality, especially from lymphoma, in adult celiac disease (CD). Although serum IgA antitransglutaminase (IgA-tTG-ab), like antiendomysium (IgA-EMA) antibodies, are sensitive and specific screening tests for untreated CD, their reliability as predictors of strict compliance to and dietary transgressions from a GFD is not precisely known. We aimed to address this question in consecutively treated adult celiacs. METHODS: In a cross-sectional study, 95 non-IgA deficient adult (median age: 41 yr) celiacs on a GFD for at least 1 yr (median: 6 yr) were subjected to 1) a dietician-administered inquiry to pinpoint and quantify the number and levels of transgressions (classified as moderate or large, using as a cutoff value the median gluten amount ingested in the overall noncompliant patients of the series) over the previous 2 months, 2) a search for IgA-tTG-ab and -EMA, and 3) perendoscopic duodenal biopsies. The ability of both antibodies to discriminate celiacs with and without detected transgressions was described using receiver operating characteristic curves and quantified as to sensitivity and specificity, according to the level of transgressions. RESULTS: Forty (42%) patients strictly adhered to a GFD, 55 (58%) had committed transgressions, classified as moderate (< or = 18 g of gluten/2 months; median number 6) in 27 and large (>18 g; median number 69) in 28. IgA-tTG-ab and -EMA specificity (proportion of correct recognition of strictly compliant celiacs) was 0.97 and 0.98, respectively, and sensitivity (proportion of correct recognition of overall, moderate, and large levels of transgressions) was 0.52, 0.31, and 0.77, and 0.62, 0.37, and 0.86, respectively. IgA-tTG-ab and -EMA titers were correlated (p < 0.001) to transgression levels (r = 0.560 and R = 0.631, respectively) and one to another (p < 0.001) in the whole patient population (r = 0.834, N = 84) as in the noncompliant (r = 0.915, N = 48) group. Specificity and sensitivity of IgA-tTG-ab and IgA-EMA for recognition of total villous atrophy in patients under a GFD were 0.90 and 0.91, and 0.60 and 0.73, respectively. CONCLUSIONS: In adult CD patients on a GFD, IgA-tTG-ab are poor predictors of dietary transgressions. Their negativity is a falsely secure marker of strict diet compliance.

Revising Justice: Punitory Thought and Action in the Work of Atwood, Jordan, and Oates

*Designated as an exemplary master's project for 2015-16*