@misc{Schuck2004,
  author    = {Schuck, Christoph},
  title     = {Der B{\"u}rgerkrieg in Aceh : Konsequenzen f{\"u}r den Weg Indonesiens zur Demokratie},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-9647},
  year      = {2004},
  abstract  = {Indonesia's arduous path to democracy is threatened by several domestic conflicts. Although the civil war in Aceh - a region in the north of Sumatra - has claimed thousands of victims, the incidents have not yet been adequately dealt with - neither in the public domain nor within the scientific community. In May 2003, the Indonesian president, Megawati Sukarnoputri, imposed material law on the Aceh region in order to crack down on the separatist movement Gerakan Aceh Merdeka (GAM). This step does not seem to be in line with serious concepts of democracy and is threatening the consolidation of the transformation process. The author seeks to shed light on the roots of the conflict, the motivation of leading politicians in Jakarta to deploy military means instead of continuing negotiations, and its consequences for the Indonesian process of democratisation.},
  language  = {de}
}
@misc{SchuckSchleicherJanssenetal.2020,
  author    = {Schuck, Bernhard and Schleicher, Anja Maria and Janssen, Christoph and Toy, Virginia G. and Dresen, Georg},
  title     = {Fault zone architecture of a large plate-bounding strike-slip fault},
  series = {Zweitver{\"o}ffentlichungen der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe},
  journal   = {Zweitver{\"o}ffentlichungen der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe},
  number    = {1},
  issn      = {1866-8372},
  doi       = {10.25932/publishup-51244},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-512441},
  pages     = {32},
  year      = {2020},
  abstract  = {New Zealand's Alpine Fault is a large, platebounding strike-slip fault, which ruptures in large (M-w > 8) earthquakes. We conducted field and laboratory analyses of fault rocks to assess its fault zone architecture. Results reveal that the Alpine Fault Zone has a complex geometry, comprising an anastomosing network of multiple slip planes that have accommodated different amounts of displacement. This contrasts with the previous perception of the Alpine Fault Zone, which assumes a single principal slip zone accommodated all displacement. This interpretation is supported by results of drilling projects and geophysical investigations. Furthermore, observations presented here show that the young, largely unconsolidated sediments that constitute the footwall at shallow depths have a significant influence on fault gouge rheological properties and structure.},
  language  = {en}
}
@article{SchuckSchleicherJanssenetal.2020,
  author    = {Schuck, Bernhard and Schleicher, Anja Maria and Janssen, Christoph and Toy, Virginia G. and Dresen, Georg},
  title     = {Fault zone architecture of a large plate-bounding strike-slip fault},
  series = {Solid Earth},
  volume    = {11},
  journal   = {Solid Earth},
  number    = {1},
  publisher = {Copernicus Publications},
  address   = {G{\"o}ttingen},
  issn      = {1869-9529},
  doi       = {10.5194/se-11-95-2020},
  pages     = {95 -- 124},
  year      = {2020},
  abstract  = {New Zealand's Alpine Fault is a large, platebounding strike-slip fault, which ruptures in large (M-w > 8) earthquakes. We conducted field and laboratory analyses of fault rocks to assess its fault zone architecture. Results reveal that the Alpine Fault Zone has a complex geometry, comprising an anastomosing network of multiple slip planes that have accommodated different amounts of displacement. This contrasts with the previous perception of the Alpine Fault Zone, which assumes a single principal slip zone accommodated all displacement. This interpretation is supported by results of drilling projects and geophysical investigations. Furthermore, observations presented here show that the young, largely unconsolidated sediments that constitute the footwall at shallow depths have a significant influence on fault gouge rheological properties and structure.},
  language  = {en}
}