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

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.

@inproceedings{id631,
  address = {Graz, Austria},
  author = {Kraft, T. and Wassermann, J. and Igel, H.   and Schmedes, E.},
  booktitle = {DDG, 65. Jahrestagung},
  language = {en},
  title = {The 2002 Hochstaufen, SE-Germany, earthquake swarm: Cluster analysis and high precision event location},
  volume = {SOp17},
  year = {2005},
}

%O Conference Proceedings
%C Graz, Austria
%A Kraft, T.
%A Wassermann, J.
%A Igel, H.  
%A Schmedes, E.
%B DDG, 65. Jahrestagung
%G en
%T The 2002 Hochstaufen, SE-Germany, earthquake swarm: Cluster analysis and high precision event location
%V SOp17
%D 2005