@misc{HiemerRoesslerScherbaum2010,
  author    = {Hiemer, Stefan and R{\"o}ßler, Dirk and Scherbaum, Frank},
  title     = {Catalog of Swarm Earthquakes in Vogtland /West Bohemia in 2008/09},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-53837},
  year      = {2010},
  abstract  = {The document contains the catalog of earthquakes in Vogtland /West Bohemia within the period of 2008/10/19 -to- 2009/03/16. The events were recorded by a seismic mini-array operated by the Institute of Earthsciences, University of Postdam.},
  language  = {en}
}
@misc{HiemerRoesslerScherbaum2010,
  author    = {Hiemer, Stefan and R{\"o}ßler, Dirk and Scherbaum, Frank},
  title     = {Catalog of Swarm Earthquakes in Vogtland /West Bohemia in 2008/09},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-51710},
  year      = {2010},
  abstract  = {The document contains the catalog of earthquakes in Vogtland /West Bohemia within the period of 2008/10/19 -to- 2009/03/16. The events were recorded by a seismic mini-array operated by the Institute of Earthsciences, University of Postdam.},
  language  = {en}
}
@misc{RoesslerHiemerBachetal.2009,
  author    = {R{\"o}ßler, Dirk and Hiemer, Stephan and Bach, Christoph and Delavaud, Elise and Kr{\"u}ger, Frank and Ohrnberger, Matthias and Sauer, David and Scherbaum, Frank and Vollmer, Daniel},
  title     = {Small-aperture seismic array monitors Vogtland earthquake swarm in 2008/09},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-29185},
  year      = {2009},
  abstract  = {The most recent intense earthquake swarm in the Vogtland lasted from 6 October 2008 until January 2009. Greatest magnitudes exceeded M3.5 several times in October making it the greatest swarm since 1985/86. In contrast to the swarms in 1985 and 2000, seismic moment release was concentrated near swarm onset. Focal area and temporal evolution are similar to the swarm in 2000. Work hypothysis: uprising upper-mantle fluids trigger swarm earthquakes at low stress level. To monitor the seismicity, the University of Potsdam operated a small aperture seismic array at 10 km epicentral distance between 18 October 2008 and 18 March 2009. Consisting of 12 seismic stations and 3 additional microphones, the array is capable of detecting earthquakes from larger to very low magnitudes (M<-1) as well as associated air waves. We use array techniques to determine properties of the incoming wavefield: noise, direct P and S waves, and converted phases.},
  language  = {en}
}