@misc{PassarelliHainzlCescaetal.2016,
  author    = {Passarelli, Luigi and Hainzl, Sebastian and Cesca, Simone and Maccaferri, Francesco and Mucciarelli, Marco and Roessler, Dirk and Corbi, Fabio and Dahm, Torsten and Rivalta, Eleonora},
  title     = {Aseismic transient driving the swarm-like seismic sequence in the Pollino range, Southern Italy (vol 201, pg 1553, 2015)},
  series = {Geophysical journal international},
  volume    = {204},
  journal   = {Geophysical journal international},
  publisher = {Oxford Univ. Press},
  address   = {Oxford},
  issn      = {0956-540X},
  doi       = {10.1093/gji/ggv425},
  pages     = {365 -- 365},
  year      = {2016},
  language  = {en}
}
@article{DonnerKruegerRoessleretal.2014,
  author    = {Donner, Stefanie and Kr{\"u}ger, Frank and Roessler, Dirk and Ghods, Abdolreza},
  title     = {Combined Inversion of broadband and short-period waveform data for regional moment tensors: A case study in the Alborz Mountains, Iran},
  series = {Bulletin of the Seismological Society of America},
  volume    = {104},
  journal   = {Bulletin of the Seismological Society of America},
  number    = {3},
  publisher = {Seismological Society of America},
  address   = {Albany},
  issn      = {0037-1106},
  doi       = {10.1785/0120130229},
  pages     = {1358 -- 1373},
  year      = {2014},
  abstract  = {In this study, we suggest a novel approach for the retrieval of regional moment tensors for earthquakes with small to moderate magnitudes. The first modification is the combined inversion of broadband and short-period waveform data. The broadband waveforms are inverted in a frequency range suitable for surface waves, whereas for the short-period data a frequency range suitable for body waves is applied. The second modification is the use of first-motion body-wave polarities to select the most probable solution out of all solutions from inversion. To combine three different criteria for selecting the most probable solution (i.e., residual from inversion, double-couple content of solution, number of nonmatching first-motion body-wave polarities), the L2 norm is applied to the normalized parameters. We chose five earthquakes within the Alborz mountains, Iran, as a case study (3.1 <= M-w <= 4.1). In this area, several factors exacerbate the difficulty of performing inversion for moment tensors, for example, a heterogeneous station network and large azimuthal gaps. We have demonstrated that our approach supplies reliable moment tensors when inversion from broadband data alone fails. In one case, we successfully retrieved a stable solution from short-period waveform data alone. Thus, our approach enables successful determination of seismic moment tensors wherever a sparse network of broadband stations has thus far prevented it.},
  language  = {en}
}