Search for Dark Matter in events with a highly energetic jet and missing transverse momentum in proton-proton collisions at root out s = 8 TeV with the ATLAS detector

The experiments at the Large Hadron Collider at the European Centre for Particle Physics, CERN, rely on efficient and reliable trigger systems for singling out interesting events. This thesis documents two online timing monitoring tools for the central trigger of the ATLAS experiment as well as the adaption of the central trigger simulation as part of the upgrade for the second LHC run. Moreover, a search for candidates for so-called Dark Matter, for which there is ample cosmological evidence, is presented. This search for generic weakly interacting massive particles (WIMPs) is based on the roughly 20/fb of proton-proton collisions at a centre-of-mass-energy of sqrt{s}=8 TeV recorded with the ATLAS detector in 2012. The considered signature are events with a highly energetic jet and large missing transverse energy. No significant deviation from the theory prediction is observed. Exclusion limits are derived on parameters of different signal models and compared to the results of other experiments. Finally, the results of a simulation study on the potential of the analysis at sqrt{s}=14 TeV are presented.

UHP metamorphic rocks of the Eastern Rhodope Massif, NE Greece: new constraints from petrology, geochemistry and zircon ages

In this PhD thesis, a multidisciplinary study has been carried out on metagranitoids and paragneisses from the Eastern Rhodope Massif, northern Greece, to decipher the pre-Alpine magmatic and geodynamic evolution of the Rhodope Massif and to correlate the eastern part with the western/central parts of the orogen. The Rhodope Massif, which occupies the major part of NE Greece and S Bulgaria, represents the easternmost part of the Internal Hellenides. It is regarded as a nappe stack of high-grade units, which is classically subdivided into an upper unit and a lower unit, separated by a SSE-NNW trending thrust plane, the Nestos thrust. Recent research in the central Greek Rhodope Massif revealed that the two units correspond to two distinct terranes of different age, the Permo-Carboniferous Thracia Terrane, which was overthrusted by the Late Jurassic/Early Cretaceous Rhodope Terrane. These terranes are separated by the Nestos suture, a composite zone comprising metapelites, metabasites, metagranitoids and marbles, which record high-pressure and even ultrahigh-pressure metamorphism in places. Similar characteristic rock associations were investigated during this study along several well-constrained cross sections in vincity to the Ada, Sidiro and Kimi villages in the Greek Eastern Rhodope Massif. Field evidence revealed that the contact zone of the two terranes in the Eastern Rhodope Massif is characterized by a mélange of metapelites, migmatitic amphibolites/eclogites, strongly sheared orthogneisses and marbles. The systematical occurrence of this characteristic rock association between the terranes implies that the Nestos suture is a continuous belt throughout the Greek Rhodope Massif. In this study, a new UHP locality could be established and for the first time in the Greek Rhodope, metamorphic microdiamonds were identified in situ in their host zircons using Laser-Raman spectroscopy. The presence of the diamonds as well as element distribution patterns of the zircons, obtained by TOF-SIMS, indicate metamorphic conditions of T > 1000 °C and P > 4 GPa. The high-pressure and ultrahigh-pressure rocks of the mélange zone are considered to have formed during the subduction of the Nestos Ocean in Jurassic times at ~150 Ma. Melting of metapelitic rocks at UHP conditions facilitated the exhumation to lower crustal levels. To identify major crust forming events, basement granitoids were dated by LA-SF-ICPMS and SHRIMP-II U-Pb analyses of zircons. The geochronological results revealed that the Eastern Rhodope Massif consists of two crustal units, a structurally lower Permo-Carboniferous unit corresponding to the Thracia Terrane and a structurally upper Late Jurassic/Early Cretaceous unit corresponding to the Rhodope Terrane, like it was documented for the Central Rhodope Massif. Inherited zircons in the orthogneisses from the Thracia Terrane of the Eastern Rhodope Massif indicate the presence of a pre-existing Neoproterozoic and Ordovician-Silurian basement in this region. Triassic magmatism is witnessed by the zircons of few orthogneisses from the easternmost Rhodope Massif and is interpreted to be related to rifting processes. Whole-rock major and trace element analyses indicate that the metagranitoids from both terranes originated in a subduction-related magmatic-arc environment. The Sr-Nd isotope data for both terranes of the Eastern and Central Rhodope Massif suggest a mixed crust-mantle source with variable contributions of older crustal material as already indicated by the presence of inherited zircons. Geochemical and isotopic similarity of the basement of the Thracia Terrane and the Pelagonian Zone implies that the Thracia Terrane is a fragment of a formerly unique Permo-Carboniferous basement, separated by rifting and opening of the Meliata-Maliac ocean system in Triassic times. A branch of the Meliata-Maliac ocean system, the Nestos Ocean, subducted northwards in Late Jurassic times leading to the formation of the Late Jurassic/Early Cretaceous Rhodope magmatic arc on remnants of the Thracia Terrane as suggested by inherited Permo-Carboniferous zircons. The ~150 Ma zircon ages of the orthogneisses from the Rhodope Terrane indicate that subduction-related magmatism and HP/UHP metamorphism occurred during the same subduction phase. Subduction ceased due to the closure of the Nestos Ocean in the Late Jurassic/Early Cretaceous. The post-Jurassic evolution of the Rhodope Massif is characterized by the exhumation of the Rhodope core complex in the course of extensional tectonics associated with late granite intrusions in Eocene to Miocene times.

Fremder Bruder: die Teilungssituation zwischen Süd- und Nordkorea im Spiegel des koreanischen Films seit dem Korea-Krieg

Als charakteristische Besonderheit in der koreanischen Geschichte besitzt der Korea-Krieg eine wichtige Position, so dass er bisher die gesamte Landesstruktur und -geschichte stark beeinflusst hat. Das gilt auch für die koreanische Filmgeschichte und nach dem Korea-Krieg im Jahr 1950 wurde in den Filmen das Thema „Landesteilung“ häufig aufgegriffen und bis heute oft behandelt.rnIn dieser Untersuchung werden solche Filme als Konflikt-Filme bezeichnet, die die Spaltung des Landes und die Beziehungen zu Nordkorea thematisieren, und insgesamt 60 Beispielfilme aus verschiedenen Filmgenres seit dem Ende des Korea-Kriegs bis zur Gegenwart analysiert und unter dem Aspekt beleuchtet, wie diese politischen und gesellschaftlichen Themen über das Verhältnis zwischen Süd- und Nordkorea repräsentiert werden. Mit Hilfe von Beispielfilmen wird versucht, herauszufinden, wie stark und unterschiedlich der Bruderkrieg und die davon abgeleitete Teilung des Landes in südkoreanischen Filmen im Wandel der Geschichte widergespiegelt werden. rnDiese Arbeit setzt sich zuerst mit Kracauers Spiegeltheorie, einer filmsoziologischen Theorie, und der Genretheorie als wichtigen theoretischen Überlegungen auseinander, um zu verdeutlichen, in welchem Bezug Konfliktfilme über die südkoreanische Gesellschaft angesehen werden und welche Rolle sie als Spiegel der Gesellschaft spielen, um gesellschaftliche Stimmungen, Bewusstseinsformen und Wünsche zu verdeutlichen. Dabei werden die kulturellen und gesellschaftlichen sowie filmwirtschaftlichen Aspekte berücksichtigt. rnDie vorliegende Arbeit bietet einen umfangreichen Überblick über den Konfliktfilm im südkoreanischen Kino seit dem Korea-Krieg. Die koreanischen Konflikt-Filme als regional-spezifische Filmkategorie stehen im engen Zusammenhang mit dieser politischen Situation und die Darstellung sowie Thematisierung Nordkoreas werden jeweils durch die verschiedenen Generationen der Filmemacher unterschiedlich präsentiert. Im südkoreanischen Diskurs bilden sie ein eigenes Genre, das alle klassischen und gemischten Filmgenres integriert; im Wandel der Geschichte haben sie sich dabei stetig weiterentwickelt, in engem Zusammenhang mit der Politik der verschiedenen Präsidenten Südkoreas gegenüber Nordkorea. rn