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The 2002 Hochstaufen, SE-Germany, earthquake swarm: Cluster analysis and high precision event location

Kraft, T., J. Wassermann, H. Igel, and E. Schmedes (2005), The 2002 Hochstaufen, SE-Germany, earthquake swarm: Cluster analysis and high precision event location, in DDG, 65. Jahrestagung, vol. SOp17, Graz, Austria.

Abstract
Earthquake swarms are thought to result from the interaction of subsurface fluids and the earth's crust. Our seismo-meteorological monitoring network observed two rainfall-induced swarm earthquake sequences. We review the observations and present first results of cluster analysis and relocation of the seismicity using a joint inversion of absolute, catalog differential and cross-correlated differential arrival times.
BibTeX
@inproceedings{id631,
  address = {Graz, Austria},
  author = {T. Kraft and J. Wassermann and H.   Igel and E. Schmedes},
  booktitle = {DDG, 65. Jahrestagung},
  title = {{The 2002 Hochstaufen, SE-Germany, earthquake swarm: Cluster analysis and high precision event location}},
  volume = {SOp17},
  year = {2005},
}
EndNote
%A Kraft, T.
%A Wassermann, J.
%A Igel, H.  
%A Schmedes, E.
%D 2005
%V SOp17
%T The 2002 Hochstaufen, SE-Germany, earthquake swarm: Cluster analysis and high precision event location
%C Graz, Austria
%B DDG, 65. Jahrestagung
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Printed 25. Aug 2019 09:12