Tierärztl. Hochsch., Diss., 2002--Hannover.

Thesis (D.M.A.)--Ohio State University, 2007. / Title from first page of PDF file. Includes bibliographical references (p. 126-129).

Diss.--Neuphilologische Fakultät--Universität Tübingen, 1994. / Bibliogr. p. 160-181.

Texte remanié de: Proefschrift--Rijksuniversiteit te Utrecht, 1993. / Bibliogr. p. 311-323. Index.

abstract: The San Andreas Fault (SAF) is the primary structure within a system of faults accommodating motion between the North American and Pacific plates. Physical models of faulting and characterizations of seismic hazard are informed by investigations of paleoseismology, slip distribution, and slip rate. The impact of earthquakes on people is due in large part to social vulnerability. This dissertation contributes an analysis about the relationships between earthquake hazard and social vulnerability in Los Angeles, CA and investigations of paleoseismology and fault scarp array complexity on the central SAF. Analysis of fault scarp array geometry and morphology using 0.5 m digital elevation models along 122 km of the central SAF reveals significant variation in the complexity of SAF structure. Scarp trace complexity is measured by scarp separation, changes in strike, fault trace gaps, and scarp length per SAF kilometer. Geometrical complexity in fault scarp arrays indicates that the central SAF can be grouped into seven segments. Segment boundaries are controlled by interactions with subsidiary faults. Investigation of an offset channel at Parkfield, CA yields a late Holocene slip rate of 26.2 +6.4/- 4.3 mm/yr. This rate is lower than geologic measurements on the Carrizo section of the SAF and rates implied by far-field geodesy. However, it is consistent with historical observations of slip at Parkfield. Paleoseismology at Parkfield indicates that large earthquakes are absent from the stratigraphic record for at least a millennia. Together these observations imply that the amount of plate boundary slip accommodated by the main SAF varies along strike. Contrary to most environmental justice analyses showing that vulnerable populations are spatially-tied to environmental hazards, geospatial analyses relating social vulnerability and earthquake hazard in southern California show that these groups are not disproportionately exposed to the areas of greatest hazard. Instead, park and green space is linked to earthquake hazard through fault zone regulation. In Los Angeles, a parks poor city, the distribution of social vulnerability is strongly tied to a lack of park space. Thus, people with access to financial and political resources strive to live in neighborhoods with parks, even in the face of forewarned risk. / Dissertation/Thesis / Ph.D. Geological Sciences 2011

This study of alluvial aquifer basins in southern California is centered on observations of differential surface displacement and the search for the mechanisms of deformation. The San Bernardino basin and the Upper Coachella Valley aquifers are bound by range fronts and fault segments of the southern San Andreas fault system. I have worked to quantify long-term compaction in these groundwater dependent population centers with a unique synthesis of data and methodologies using Interferometric Synthetic Aperture Radar (InSAR) and groundwater data. My dissertation contributes to the understanding of alluvial aquifer heterogeneity and partitioning. I model hydrogeologic and tectonic interpretations of deformation where decades of overdraft conditions and ongoing aquifer development contribute to extreme rapid subsidence. I develop the Hydrogeologic InSAR Integration (HII) method for the characterization of surface deformation in aquifer basins. The method allows for the separation of superimposed hydraulic and/or tectonic processes in operation. This formalization of InSAR and groundwater level integration provides opportunities for application in other aquifer basins where overdraft conditions may be causing permanent loss of aquifer storage capacity through compaction. Sixteen years of SAR data for the Upper Coachella Valley exhibit rapid vertical surface displacement (#8804; 48mm/a) in sharply bound areas of the western basin margin. Using well driller logs, I categorize a generalized facies analysis of the western basin margin, describing heterogeneity of the aquifer. This allowed for assessment of the relationships between observed surface deformation and sub-surface material properties. Providing the setting and context for the hydrogeologic evolution of California's primary aquifers, the mature San Andreas transform fault is studied extensively by a broad range of geoscientists. I present a compilation of observations of creep, line integrals across the Pacific-North America Plate Boundary, and strain tensor volumes for comparison to the Working Group 2007 (UCERF 2) seismicity-based deformation model. I find that the moment accumulation across the plate boundary is consistent with the deformation model, suggesting fault displacement observations within the plate boundary zone accurately capture the strain across the plate boundary. This dissertation includes co-authored materials previously published, and also includes unpublished work currently under revisions for submission to a technical journal.

Sedimentary rocks in the Mecca Hills record a 3-4 Myr history of basin evolution and deformation within the southern San Andreas fault (SAF) zone. Detailed geologic mapping, measured sections, lithofacies analysis, and preliminary paleomagnetic data indicate that sedimentation and deformation in the Mecca Hills resulted from evolution of local fault zone complexities superimposed on regional subsidence and uplift. Sediment was derived from sources northeast of the SAF and transported southeast along the fault zone in large rivers, alluvial fans, and a smaller fault-bounded lake. Inversion of the Painted Canyon fault from oblique SW-side down to SW-side up slip was the main control on local deposition and deformation. Regional controls are suggested by an angular unconformity observed in the Mecca and Indio Hills along ~50 km of the SAF and synchronous post-740 ka uplift northeast of the SAF along ~80 km of the fault zone.

Detta arbete är skapat av Andreas Bartziokas, som examensarbete för VT 2009. I denna uppsats beskrivs hur spelet B.O.B. har skapats. Vilken litteratur som varit användbar för skapandet av spelet, samt en övergripande beskrivning av själva spelet.

Um den deutschen Barock zu verstehen, beginnen wir mit einer Erklärung de sozio-kulturellen und politischen Voraussetungen, die zum Dreissigjährigen Krieg führten und ihre Beziehung zu dem wichtigsten Dichter der Zeit, Andreas Gryphius. Ausserdem wird das Werk des Dichters im Hinblick auf das Repräsentationsmodell im 17. Jahrhundert untersucht, insbesondere seine Sonette. / Para compreender o Barroco alemão iniciaremos uma explanação dos pressupostos sócio-culturais e políticos que levaram à Guerra dos Trinta Anos e sua relação com o poeta mais expressivo do momento, Andreas Gryphius. Além disso, a obra do poeta será analisada a partir do modelo de representação que havia na sociedade do século XVII, em especial em seus sonetos

This paper applies the ethnic boundary making theory developed by Andreas Wimmer to understand the maintenance of Jewish ethnic identification in Sweden, as expressed in thirteen interviews with Swedish Jews. Wimmer’s theory holds that ethnic conflict and persecution routinizes and entrenches perceptions of ethnic difference; I argue that the antisemitic persecutions of the 20th century has entrenched the perception of the ethnic distinctiveness of Jews among Jews themselves. These persecutions also contribute to alienation from Swedish society, which does not share the same historical identity and frames of understanding. These factors in turn motivate the participants to maintain the ethnic boundary between Swedes and Jews and guard it against assimilation. Ethnic consciousness also motivates Jews to endow the category of “Jewish” with cultural content, sometimes having previously lacked knowledge of Jewish culture; the cultural distinctiveness of Jews is thus shown to partly be a result of the ethnic boundary between Jews and others, and not just an explanation for that boundary. However; the participants are generally not prepared to restrict the choice of romantic bonds to fellow Jews; since social closure is required to maintain ethnic boundaries (as stressed by Wimmer), this puts the participants in a contradictory situation.