@article{HoffmannSiehr1998,
  author    = {Hoffmann, Michael and Siehr, Karl-Heinz},
  title     = {Alles eine Frage des Stils? : Aspekte von Sprachvariation am Beispiel Jugendsprache},
  year      = {1998},
  language  = {de}
}
@article{WeberAbuAyyashAbueladasetal.2009,
  author    = {Weber, Michael H. and Abu-Ayyash, Khalil and Abueladas, Abdel-Rahman and Agnon, Amotz and Alasonati-Taš{\´a}rov{\´a}, Zuzana and Al-Zubi, Hashim and Babeyko, Andrey and Bartov, Yuval and Bauer, Klaus and Becken, Michael and Bedrosian, Paul A. and Ben-Avraham, Zvi and Bock, G{\"u}nter and Bohnhoff, Marco and Bribach, Jens and Dulski, Peter and Ebbing, Joerg and El-Kelani, Radwan J. and Foerster, Andrea and F{\"o}rster, Hans-J{\"u}rgen and Frieslander, Uri and Garfunkel, Zvi and G{\"o}tze, Hans-J{\"u}rgen and Haak, Volker and Haberland, Christian and Hassouneh, Mohammed and Helwig, Stefan L. and Hofstetter, Alfons and Hoffmann-Rothe, Arne and Jaeckel, Karl-Heinz and Janssen, Christoph and Jaser, Darweesh and Kesten, Dagmar and Khatib, Mohammed Ghiath and Kind, Rainer and Koch, Olaf and Koulakov, Ivan and Laske, Maria Gabi and Maercklin, Nils},
  title     = {Anatomy of the Dead Sea transform from lithospheric to microscopic scale},
  issn      = {8755-1209},
  doi       = {10.1029/2008rg000264},
  year      = {2009},
  abstract  = {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.},
  language  = {en}
}
@misc{VoigtZimmermannStierLascheitetal.2019,
  author    = {Voigt-Zimmermann, Susanne and Stier, Karl-Heinz and Lascheit, Thomas and Kruse, Stephanie A. and Blickensdorff, Maria and F{\"o}rster, Theresa and Schumacher, Rebecca and Burchert, Frank and Ablinger, Irene and F{\"o}rster, Christine and Wahl, Michael and Schirmacher, Irene and Ostermann, Frank and Welke, Lisa-Marie and Frank, Ulrike and Zakari{\´a}s, Lilla and Salis, Christos and Wartenburger, Isabell and Krug, Ragna and St{\"u}bner, Hanna and Hoffmann, Sophie and Heide, Judith},
  title     = {Spektrum Patholinguistik Band 11. Schwerpunktthema: Gut gestimmt: Diagnostik und Therapie bei Dysphonie},
  number    = {11},
  editor    = {Fritzsche, Tom and Yetim, {\"O}zlem and Otto, Constanze and Adelt, Anne},
  publisher = {Universit{\"a}tsverlag Potsdam},
  address   = {Potsdam},
  isbn      = {978-3-86956-448-7},
  issn      = {1866-9085},
  doi       = {10.25932/publishup-41857},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-418574},
  pages     = {142},
  year      = {2019},
  abstract  = {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 j{\"a}hrlich vom Verband f{\"u}r Patholinguistik e.V. (vpl) durchgef{\"u}hrt. Der vorliegende Tagungsband beinhaltet die Hauptvortr{\"a}ge zum Schwerpunktthema sowie Beitr{\"a}ge zu den Kurzvortr{\"a}gen »Spektrum Patholinguistik« und der Posterpr{\"a}sentationen zu weiteren Themen aus der sprachtherapeutischen Forschung und Praxis.},
  language  = {de}
}
@book{SiehrKernHoffmannetal.2016,
  author    = {Siehr, Karl-Heinz and Kern, Friederike and Hoffmann, Michael and Großbr{\"o}hmer, Christoph and M{\"u}hlbauer, Evelyn and Berner, Elisabeth and Leubner, Martin and Friese, Antonia and Preis, Matthias and Josting, Petra and H{\"o}fner, Marion and Schepe, Kerstin},
  title     = {Sport als Thema im Deutschunterricht},
  editor    = {Kern, Friederike and Siehr, Karl-Heinz},
  publisher = {Universit{\"a}tsverlag Potsdam},
  address   = {Potsdam},
  isbn      = {978-3-86956-381-7},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-95307},
  publisher      = {Universit{\"a}t Potsdam},
  year      = {2016},
  abstract  = {Ein Deutschunterricht, der die Alltags- und Medienkultur der Sch{\"u}ler und Sch{\"u}lerinnen ernst nimmt, darf Sporttexte nicht unber{\"u}cksichtigt lassen. Zu sehr ist der Sport in all seinen Facetten Teil der Lebenswelt vieler Sch{\"u}lerinnen und Sch{\"u}ler 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 Bez{\"u}gen zwischen Sport und Deutschunterricht schon seit l{\"a}ngerem intensiv betrieben wird, offenbart das vielschichtige Kulturph{\"a}nomen „Sport" immer wieder neue interessante Seiten, die es lohnen, fachdidaktisch behandelt zu werden. Die zehn Beitr{\"a}ge in diesem Band verstehen sich als Unterrichtsanregungen f{\"u}r 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 f{\"u}r das Verst{\"a}ndnis erforderlich sind. Im Zentrum vieler Beitr{\"a}ge stehen Unterrichtsszenarien mit kommentierten Texten und Aufgaben, die f{\"u}r die Unterrichtsvorbereitung oder f{\"u}r den Unterricht selbst genutzt werden k{\"o}nnen.},
  language  = {de}
}
@book{AlbersAppelBaueretal.2008,
  author    = {Albers, Marion and Appel, Ivo and Bauer, Hartmut and von Bogdandy, Armin and Britz, Gabriele and Bumke, Wolfgang and Fehling, Michael and Gusy, Christoph and Hermes, Georg and Hill, Hermann and Hoffmann-Riem, Wolfgang and Holznagel, Bernd and K{\"o}ck, Wolfgang and Ladeur, Karl-Heinz and Michael, Lothar and Pitschas, Rainer and R{\"o}hl, Hans Christian and Rossen-Stahlfeld, Helge and Sachs, Michael and Sachsofsky, Ute and Schmidt-Aßmann, Eberhard and Schneider, Jens-Peter and Vesting, Thomas},
  title     = {Grundlagen des Verwaltungsrechts : Bd. II Informationsordnung, Verwaltungsverfahren, Handlungsformen},
  volume    = {2},
  editor    = {Hoffmann-Riem, Wolfgang and Schmidt-Aßmann, Eberhard and Voßkuhle, Andreas},
  publisher = {Beck},
  address   = {M{\"u}nchen},
  isbn      = {978-3-406-54718-8},
  pages     = {1712 S.},
  year      = {2008},
  language  = {de}
}
@article{HeitYuanWeberetal.2015,
  author    = {Heit, Benjamin and Yuan, Xiaohui and Weber, Michael H. and Geissler, Wolfram H. and Jokat, Wilfried and Lushetile, Bufelo and Hoffmann, Karl-Heinz},
  title     = {Crustal thickness and V-p/V-s ratio in NW Namibia from receiver functions: Evidence for magmatic underplating due to mantle plume-crust interaction},
  series = {Geophysical research letters},
  volume    = {42},
  journal   = {Geophysical research letters},
  number    = {9},
  publisher = {American Geophysical Union},
  address   = {Washington},
  issn      = {0094-8276},
  doi       = {10.1002/2015GL063704},
  pages     = {3330 -- 3337},
  year      = {2015},
  abstract  = {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.},
  language  = {en}
}