Moment tensor catalogue of earthquakes in West Bohemia from 2008 to 2018
We present a unique catalogue of full moment tensors (MTs) of earthquakes with ML between 0.5 and 4.4 that occurred in West Bohemia, Czech Republic, in the period from 2008 to 2018 (Vavryčuk et al., 2022a, b). The MTs were calculated from vertical components of P-wave amplitudes. The MT inversion wa...
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Veröffentlicht in: | Earth system science data 2022-05, Vol.14 (5), p.2179-2194 |
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Zusammenfassung: | We present a unique catalogue of full moment tensors (MTs) of earthquakes
with ML between 0.5 and 4.4 that occurred in West Bohemia, Czech
Republic, in the period from 2008 to 2018 (Vavryčuk et al., 2022a, b). The MTs were calculated from
vertical components of P-wave amplitudes. The MT inversion was based on
principal component analysis applied to optimally filtered velocity records
of local seismic stations deployed in the West Bohemia area. The minimum
number of inverted stations is 15, and the rms between theoretical and
observed amplitudes is lower than 0.5. The catalogue is exceptional in
several aspects: (1) it represents an extraordinary, extensive dataset of
more than 5100 MTs; (2) it covers a long period of seismicity in the
studied area, during which several prominent earthquake swarms took place;
(3) the locations and retrieved MTs of earthquakes are of a high accuracy.
Additionally, we provide three-component records at the West Bohemia
(WEBNET) seismic stations, the velocity model in the region, and the
technical specification of the stations. The dataset is ideal for being
utilized by a large community of researchers for various seismological
purposes, e.g. for studies of (1) the migration of foci and the
spatiotemporal evolution of seismicity, (2) redistribution of stress during
periods of intense seismicity, (3) the interaction of faults, (4) the
Coulomb stress along the faults and local stress anomalies connected to
fault irregularities, (5) diffusivity of fluids along the activated faults,
or (6) the time-dependent seismic risk due to the migration of seismicity in
the region. In addition, the dataset is optimum for developing and testing
new inversions for MTs and for tectonic stress. Since most of the
earthquakes are non-shear, the dataset can contribute to studies of
non-double-couple components of MTs and their relation to shear–tensile
fracturing and/or seismic anisotropy in the focal zone. |
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ISSN: | 1866-3516 1866-3508 1866-3516 |
DOI: | 10.5194/essd-14-2179-2022 |