TY - JOUR A1 - Hoffmann, Michael A1 - Siehr, Karl-Heinz T1 - Alles eine Frage des Stils? : Aspekte von Sprachvariation am Beispiel Jugendsprache Y1 - 1998 ER - TY - JOUR A1 - Weber, Michael H. A1 - Abu-Ayyash, Khalil A1 - Abueladas, Abdel-Rahman A1 - Agnon, Amotz A1 - Alasonati-Tašárová, Zuzana A1 - Al-Zubi, Hashim A1 - Babeyko, Andrey A1 - Bartov, Yuval A1 - Bauer, Klaus A1 - Becken, Michael A1 - Bedrosian, Paul A. A1 - Ben-Avraham, Zvi A1 - Bock, Günter A1 - Bohnhoff, Marco A1 - Bribach, Jens A1 - Dulski, Peter A1 - Ebbing, Joerg A1 - El-Kelani, Radwan J. A1 - Foerster, Andrea A1 - Förster, Hans-Jürgen A1 - Frieslander, Uri A1 - Garfunkel, Zvi A1 - Götze, Hans-Jürgen A1 - Haak, Volker A1 - Haberland, Christian A1 - Hassouneh, Mohammed A1 - Helwig, Stefan L. A1 - Hofstetter, Alfons A1 - Hoffmann-Rothe, Arne A1 - Jaeckel, Karl-Heinz A1 - Janssen, Christoph A1 - Jaser, Darweesh A1 - Kesten, Dagmar A1 - Khatib, Mohammed Ghiath A1 - Kind, Rainer A1 - Koch, Olaf A1 - Koulakov, Ivan A1 - Laske, Maria Gabi A1 - Maercklin, Nils T1 - Anatomy of the Dead Sea transform from lithospheric to microscopic scale N2 - Fault zones are the locations where motion of tectonic plates, often associated with earthquakes, is accommodated. Despite a rapid increase in the understanding of faults in the last decades, our knowledge of their geometry, petrophysical properties, and controlling processes remains incomplete. The central questions addressed here in our study of the Dead Sea Transform (DST) in the Middle East are as follows: (1) What are the structure and kinematics of a large fault zone? (2) What controls its structure and kinematics? (3) How does the DST compare to other plate boundary fault zones? The DST has accommodated a total of 105 km of left-lateral transform motion between the African and Arabian plates since early Miocene (similar to 20 Ma). The DST segment between the Dead Sea and the Red Sea, called the Arava/Araba Fault (AF), is studied here using a multidisciplinary and multiscale approach from the mu m to the plate tectonic scale. We observe that under the DST a narrow, subvertical zone cuts through crust and lithosphere. First, from west to east the crustal thickness increases smoothly from 26 to 39 km, and a subhorizontal lower crustal reflector is detected east of the AF. Second, several faults exist in the upper crust in a 40 km wide zone centered on the AF, but none have kilometer-size zones of decreased seismic velocities or zones of high electrical conductivities in the upper crust expected for large damage zones. Third, the AF is the main branch of the DST system, even though it has accommodated only a part (up to 60 km) of the overall 105 km of sinistral plate motion. Fourth, the AF acts as a barrier to fluids to a depth of 4 km, and the lithology changes abruptly across it. Fifth, in the top few hundred meters of the AF a locally transpressional regime is observed in a 100-300 m wide zone of deformed and displaced material, bordered by subparallel faults forming a positive flower structure. Other segments of the AF have a transtensional character with small pull-aparts along them. The damage zones of the individual faults are only 5-20 m wide at this depth range. Sixth, two areas on the AF show mesoscale to microscale faulting and veining in limestone sequences with faulting depths between 2 and 5 km. Seventh, fluids in the AF are carried downward into the fault zone. Only a minor fraction of fluids is derived from ascending hydrothermal fluids. However, we found that on the kilometer scale the AF does not act as an important fluid conduit. Most of these findings are corroborated using thermomechanical modeling where shear deformation in the upper crust is localized in one or two major faults; at larger depth, shear deformation occurs in a 20-40 km wide zone with a mechanically weak decoupling zone extending subvertically through the entire lithosphere. Y1 - 2009 UR - http://www.agu.org/journals/rg/ U6 - https://doi.org/10.1029/2008rg000264 SN - 8755-1209 ER - TY - JOUR A1 - Voigt-Zimmermann, Susanne A1 - Stier, Karl-Heinz A1 - Lascheit, Thomas A1 - Kruse, Stephanie A. A1 - Blickensdorff, Maria A1 - Förster, Theresa A1 - Schumacher, Rebecca A1 - Burchert, Frank A1 - Ablinger, Irene A1 - Förster, Christine A1 - Wahl, Michael A1 - Schirmacher, Irene A1 - Ostermann, Frank A1 - Welke, Lisa-Marie A1 - Frank, Ulrike A1 - Zakariás, Lilla A1 - Salis, Christos A1 - Wartenburger, Isabell A1 - Krug, Ragna A1 - Stübner, Hanna A1 - Hoffmann, Sophie A1 - Heide, Judith ED - Fritzsche, Tom ED - Yetim, Özlem ED - Otto, Constanze ED - Adelt, Anne T1 - Spektrum Patholinguistik Band 11. Schwerpunktthema: Gut gestimmt: Diagnostik und Therapie bei Dysphonie N2 - Das 11. Herbsttreffen Patholinguistik mit dem Schwerpunktthema »Gut gestimmt: Diagnostik und Therapie bei Dysphonie« fand am 18.11.2017 in Potsdam statt. Das Herbsttreffen wird seit 2007 jährlich vom Verband für Patholinguistik e.V. (vpl) durchgeführt. Der vorliegende Tagungsband beinhaltet die Hauptvorträge zum Schwerpunktthema sowie Beiträge zu den Kurzvorträgen »Spektrum Patholinguistik« und der Posterpräsentationen zu weiteren Themen aus der sprachtherapeutischen Forschung und Praxis. N2 - The Eleventh Autumn Meeting Patholinguistics (Herbsttreffen Patholinguistik) with its main topic »Well tuned: Diagnostics and therapy in dysphonia« took place in Potsdam on November 18 2017. This annual meeting has been organised since 2007 by the Association for Patholinguistics (Verband für Patholinguistik e.V./vpl). The present proceedings contain the keynote talks on the main topic as well as contributions from the short talks in the section »Spectrum Patholinguistics« and from the poster session covering a broad range of areas in speech/language therapy research and practice. T3 - Spektrum Patholinguistik - 11 KW - Patholinguistik KW - Sprachtherapie KW - Stimmtherapie KW - Stimmstörung KW - Dysphonie KW - patholinguistics KW - speech/language therapy KW - voice therapy KW - dysphonia Y1 - 2019 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-418574 SN - 978-3-86956-448-7 SN - 1866-9085 SN - 1866-9433 IS - 11 PB - Universitätsverlag Potsdam CY - Potsdam ER - TY - BOOK A1 - Siehr, Karl-Heinz A1 - Kern, Friederike A1 - Hoffmann, Michael A1 - Großbröhmer, Christoph A1 - Mühlbauer, Evelyn A1 - Berner, Elisabeth A1 - Leubner, Martin A1 - Friese, Antonia A1 - Preis, Matthias A1 - Josting, Petra A1 - Höfner, Marion A1 - Schepe, Kerstin ED - Kern, Friederike ED - Siehr, Karl-Heinz T1 - Sport als Thema im Deutschunterricht BT - Fachliche Grundlagen – Unterrichtsanregungen – Unterrichtsmaterialien N2 - Ein Deutschunterricht, der die Alltags- und Medienkultur der Schüler und Schülerinnen ernst nimmt, darf Sporttexte nicht unberücksichtigt lassen. Zu sehr ist der Sport in all seinen Facetten Teil der Lebenswelt vieler Schülerinnen und Schüler geworden. Die Frage ist nicht mehr, ob der Deutschunterricht darauf zu reagieren hat, die Frage ist vielmehr, wie er dies tun und welche Sporttexte er dabei nutzen kann. Auch wenn die Suche nach sinnvollen Bezügen zwischen Sport und Deutschunterricht schon seit längerem intensiv betrieben wird, offenbart das vielschichtige Kulturphänomen „Sport“ immer wieder neue interessante Seiten, die es lohnen, fachdidaktisch behandelt zu werden. Die zehn Beiträge in diesem Band verstehen sich als Unterrichtsanregungen für den kompetenzorientierten Deutschunterricht. Sie bedienen Betrachtungen zum Sport aus literarischer, sprachlicher und medialer Perspektive. Die theoretisch-begrifflichen Aspekte der jeweiligen Themen werden soweit behandelt, wie sie für das Verständnis erforderlich sind. Im Zentrum vieler Beiträge stehen Unterrichtsszenarien mit kommentierten Texten und Aufgaben, die für die Unterrichtsvorbereitung oder für den Unterricht selbst genutzt werden können. KW - Deutschunterricht KW - Sportsprache KW - Varietäten KW - Sportberichterstattung KW - Medienanalyse KW - Deutschdidaktik Y1 - 2016 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-95307 SN - 978-3-86956-381-7 PB - Universitätsverlag Potsdam CY - Potsdam ER - TY - BOOK A1 - Albers, Marion A1 - Appel, Ivo A1 - Bauer, Hartmut A1 - von Bogdandy, Armin A1 - Britz, Gabriele A1 - Bumke, Wolfgang A1 - Fehling, Michael A1 - Gusy, Christoph A1 - Hermes, Georg A1 - Hill, Hermann A1 - Hoffmann-Riem, Wolfgang A1 - Holznagel, Bernd A1 - Köck, Wolfgang A1 - Ladeur, Karl-Heinz A1 - Michael, Lothar A1 - Pitschas, Rainer A1 - Röhl, Hans Christian A1 - Rossen-Stahlfeld, Helge A1 - Sachs, Michael A1 - Sachsofsky, Ute A1 - Schmidt-Aßmann, Eberhard A1 - Schneider, Jens-Peter A1 - Vesting, Thomas ED - Hoffmann-Riem, Wolfgang ED - Schmidt-Aßmann, Eberhard ED - Voßkuhle, Andreas T1 - Grundlagen des Verwaltungsrechts : Bd. II Informationsordnung, Verwaltungsverfahren, Handlungsformen Y1 - 2008 SN - 978-3-406-54718-8 VL - 2 PB - Beck CY - München ER - TY - JOUR A1 - Heit, Benjamin A1 - Yuan, Xiaohui A1 - Weber, Michael H. A1 - Geissler, Wolfram H. A1 - Jokat, Wilfried A1 - Lushetile, Bufelo A1 - Hoffmann, Karl-Heinz T1 - Crustal thickness and V-p/V-s ratio in NW Namibia from receiver functions: Evidence for magmatic underplating due to mantle plume-crust interaction JF - Geophysical research letters N2 - A seismological network was operated at the junction of the aseismic Walvis Ridge with the northwestern Namibian coast. We mapped crustal thickness and bulk V-p/V-s ratio by the H-k analysis of receiver functions. In the Damara Belt, the crustal thickness is similar to 35km with a V-p/V-s ratio of <1.75. The crust is similar to 30km thick at the coast in the Kaoko Belt. Strong variations in crustal thickness and V-p/V-s ratios are found at the landfall of the Walvis Ridge. Here and at similar to 150km northeast of the coast, the crustal thickness increases dramatically reaching 44km and the V-p/V-s ratios are extremely high (similar to 1.89). These anomalies are interpreted as magmatic underplating produced by the mantle plume during the breakup of Gondwana. The area affected by the plume is smaller than 300km in diameter, possibly ruling out the existence of a large plume head under the continent during the breakup. KW - crustal thickness KW - V-p KW - V-s ratios KW - magmatic underplating KW - Walvis Ridge KW - continental breakup Y1 - 2015 U6 - https://doi.org/10.1002/2015GL063704 SN - 0094-8276 SN - 1944-8007 VL - 42 IS - 9 SP - 3330 EP - 3337 PB - American Geophysical Union CY - Washington ER -