Articles | Volume 54
https://doi.org/10.5194/adgeo-54-129-2020
https://doi.org/10.5194/adgeo-54-129-2020
19 Nov 2020
 | 19 Nov 2020

Full-Waveform based methods for Microseismic Monitoring Operations: an Application to Natural and Induced Seismicity in the Hengill Geothermal Area, Iceland

Camilla Rossi, Francesco Grigoli, Simone Cesca, Sebastian Heimann, Paolo Gasperini, Vala Hjörleifsdóttir, Torsten Dahm, Christopher J. Bean, Stefan Wiemer, Luca Scarabello, Nima Nooshiri, John F. Clinton, Anne Obermann, Kristján Ágústsson, and Thorbjörg Ágústsdóttir

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Cited articles

Árnadóttir, T., Hreinsdóttir, S., Gudmundsson, G., Einarsson, P., Heinert, M., and Völksen, C.: Crustal deformation measured by GPS in the South Iceland Seismic Zone due to two large earthquakes in June 2000, Geophys. Res. Lett, 28, 4031–4033, https://doi.org/10.1029/2001GL013332, 2001. 
Árnason, K., Eysteinsson, H., and Hersir, G. P.: Joint 1D inversion of TEM and MT data and 3D inversion of MT data in the Hengill area, SW Iceland, Geothermics, 39, 13–34, https://doi.org/10.1016/j.geothermics.2010.01.002, 2010. 
Arnórsson, S., Axelsson, G., and Saemundsson, K.: Geothermal systems in Iceland, Jökull, 58, 269–302, 2008. 
Bessason, B., Ólafsson, E. H., Gunnarsson, G., Flóvenz, Ó. G., Jakobsdóttir, S. S., Björnsson, S., and Árnadóttir, Þ: Verklag vegna örvaðrar skjálftavirkni í jarðhitakerfum, Orkuveita Reykjavíkur, 2012. 
Böðvarsson, R., Rögnvaldsson, S. Th., Jakobsdóttir, S. S., Slunga, R., and Stefánsson, R.: The SIL data acquisition and monitoring system, Seis. Res. Lett., 67, 35–46, 1996. 
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Short summary
We investigate the microseismicity occurred at Hengill area, a complex tectonic and geothermal site, where the origin of earthquakes may be either natural or anthropogenic. We use a very dense broadband seismic monitoring network and apply full-waveform based method for location. Our results and first characterization identified different types of microseismic clusters, which might be associated to either production/injection or the tectonic activity of the geothermal area.