<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:creator>Vouillamoz, Naomi</dc:creator>
  <dc:creator>Mosar, Jon</dc:creator>
  <dc:creator>Deichmann, Nicholas</dc:creator>
  <dc:date>2017-06-01</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Seismic hazard assessment of slow active fault zones is challenging as usually only a  few decades of sparse instrumental seismic monitoring is available to characterize  seismic activity. Tectonic features linked to the observed seismicity can be mapped by  seismic imaging techniques and/or geomorphological and structural evidences. In this  study, we investigate a seismic lineament located in the Swiss Alpine foreland, which  was discussed in previous work as being related to crustal structures carrying in size  the potential of a magnitude M 6 earthquake. New, low-magnitude (−2.0 ≤ ML ≤ 2.5)  earthquake data are used to image the spatial and temporal distribution of  seismogenic features in the target area. Quantitative and qualitative analyses are  applied to the waveform dataset to better constrain earthquakes distribution and  source processes. Potential tectonic features responsible for the observed seismicity  are modelled based on new reinterpretations of oil industry seismic profiles and recent  field data in the study area. The earthquake and tectonic datasets are then integrated  in a 3D model. Spatially, the seismicity correlates over 10–15 km with a N–S oriented  sub-vertical fault zone imaged in seismic profiles in the Mesozoic cover units above a  major decollement on top of the mechanically more rigid basement and seen in  outcrops of Tertiary series east of the city of Fribourg. Observed earthquakes cluster  at shallow depth (&lt;4 km) in the sedimentary cover. Given the spatial extend of the  observed seismicity, we infer the potential of a moderate size earthquake to be  generated on the lineament. However, since the existence of along strike structures in  the basement cannot be excluded, a maximum M 6 earthquake cannot be ruled out.  Thus, the Fribourg Lineament constitutes a non-negligible source of seismic hazard in  the Swiss Alpine foreland.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/306057</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/306057/files/mos_msi.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1007/s00015-017-0269-0</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Swiss Journal of Geosciences. - 2017, vol. 110, no. 2, p. 547–563</dc:source>
  <dc:subject xmlns:ns1="xml" ns1:lang="en">Microseismicity</dc:subject>
  <dc:subject xmlns:ns2="xml" ns2:lang="en">Earthquake clustering</dc:subject>
  <dc:subject xmlns:ns3="xml" ns3:lang="en">Neotectonics</dc:subject>
  <dc:subject xmlns:ns4="xml" ns4:lang="en">Seismic imaging</dc:subject>
  <dc:subject xmlns:ns5="xml" ns5:lang="en">GIS</dc:subject>
  <dc:subject>info:eu-repo/classification/udc/55</dc:subject>
  <dc:title xmlns:ns6="xml" ns6:lang="en">Multi-scale imaging of a slow active fault zone: contribution for improved seismic hazard assessment in the Swiss Alpine foreland</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
