Pregled bibliografske jedinice broj: 948341
The variability and interpretation of earthquake source mechanisms in The Geysers geothermal field from a Bayesian standpoint based on the choice of a noise model
The variability and interpretation of earthquake source mechanisms in The Geysers geothermal field from a Bayesian standpoint based on the choice of a noise model // Journal of Geophysical Research: Solid Earth, 123 (2018), 1; 513-532 doi:10.1002/2017jb014897 (međunarodna recenzija, članak, znanstveni)
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Naslov
The variability and interpretation of earthquake source mechanisms in The Geysers geothermal field from a Bayesian standpoint based on the choice of a noise model
Autori
Mustać, Marija ; Tkalčić, Hrvoje ; Burky, Alexander L.
Izvornik
Journal of Geophysical Research: Solid Earth (2169-9313) 123
(2018), 1;
513-532
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Earthquake source ; Geothermal field ; Bayesian inversion
Sažetak
Moment tensor (MT) inversion studies of events in The Geysers geothermal field mostly focused on microseismicity and found a large number of earthquakes with significant non‐double‐couple (non‐DC) seismic radiation. Here we concentrate on the largest events in the area in recent years using a hierarchical Bayesian MT inversion. Initially, we show that the non‐DC components of the MT can be reliably retrieved using regional waveform data from a small number of stations. Subsequently, we present results for a number of events and show that accounting for noise correlations can lead to retrieval of a lower isotropic (ISO) component and significantly different focal mechanisms. We compute the Bayesian evidence to compare solutions obtained with different assumptions of the noise covariance matrix. Although a diagonal covariance matrix produces a better waveform fit, inversions that account for noise correlations via an empirically estimated noise covariance matrix account for interdependences of data errors and are preferred from a Bayesian point of view. This implies that improper treatment of data noise in waveform inversions can result in fitting the noise and misinterpreting the non‐DC components. Finally, one of the analyzed events is characterized as predominantly DC, while the others still have significant non‐DC components, probably as a result of crack opening, which is a reasonable hypothesis for The Geysers geothermal field geological setting.
Izvorni jezik
Engleski
Znanstvena područja
Geofizika
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Nature Index