Articles | Volume 5, issue 2
https://doi.org/10.5194/se-5-863-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-5-863-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
27 Aug 2014
Research article |
| 27 Aug 2014
Velocity structure and the role of fluids in the West Bohemia Seismic Zone
C. Alexandrakis
Institute of Geophysics and Geoinformatics, TU Bergakademie Freiberg, Freiberg, Germany
M. Calò
Berkeley Seismological Laboratory, Berkeley, USA
F. Bouchaala
The Petroleum Institute, Abu Dhabi, United Arabic Emirates
V. Vavryčuk
Institute of Geophysics, Czech Academy of Science, Prague, Czech Republic
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Cited
21 citations as recorded by crossref.
- Seismic tomography reveals a mid-crustal intrusive body, fluid pathways and their relation to the earthquake swarms in West Bohemia/Vogtland S. Mousavi et al. https://doi.org/10.1093/gji/ggv338
- Alteration as possible cause for transition from brittle failure to aseismic slip: the case of the NW-Bohemia / Vogtland earthquake swarm region J. Heinicke et al. https://doi.org/10.1016/j.jog.2019.01.010
- Kinematics of Crystal Growth in Single‐Seal Syntaxial Veins in Limestone ‐ A Phase‐Field Study M. Späth et al. https://doi.org/10.1029/2021JB022106
- Three-dimensional S-wave velocity model of the Bohemian Massif from Bayesian ambient noise tomography L. Valentová et al. https://doi.org/10.1016/j.tecto.2017.08.033
- Can hydroseismicity explain recurring earthquake swarms in NW-Bohemia? J. Heinicke et al. https://doi.org/10.1093/gji/ggx412
- ICDP drilling of the Eger Rift observatory: magmatic fluids driving the earthquake swarms and deep biosphere T. Fischer et al. https://doi.org/10.5194/sd-31-31-2022
- Tears, windows, and signature of transform margins on slabs. Images of the Cocos plate fragmentation beneath the Tehuantepec isthmus (Mexico) using Enhanced Seismic Models M. Calò https://doi.org/10.1016/j.epsl.2021.116788
- Clustering of 2008 West Bohemian seismic swarm mechanisms and its possible interpretation P. Kolar https://doi.org/10.13168/AGG.2018.0001
- Wadati method as a simple tool to study seismically active fault zones: a case study from the West-Bohemia/Vogtland region, central Europe O. Novotný et al. https://doi.org/10.1007/s11200-015-1206-1
- Event couple spectral ratio Q method for earthquake clusters: application to northwest Bohemia M. Kriegerowski et al. https://doi.org/10.5194/se-10-317-2019
- Anatomy of the Campi Flegrei caldera using Enhanced Seismic Tomography Models M. Calò & A. Tramelli https://doi.org/10.1038/s41598-018-34456-x
- Focal Mechanisms of West Bohemia, Central Europe, Earthquakes—End of May 2014: Evidence of Volume Changes D. Křížová & J. Málek https://doi.org/10.1785/0220200389
- Automated microseismic event location using Master-Event Waveform Stacking F. Grigoli et al. https://doi.org/10.1038/srep25744
- Geophysical characterization of the Cerro Machin geothermal area using three dimensional seismic and resistivity models J. Herrera & M. Calò https://doi.org/10.1016/j.geothermics.2025.103370
- CO2 degassing in the Hartoušov mofette area, western Eger Rift, imaged by CO2 mapping and geoelectrical and gravity surveys T. Nickschick et al. https://doi.org/10.1007/s00531-014-1140-4
- Shallow crustal discontinuities inferred from waveforms of microearthquakes: Method and application to KTB Drill Site and West Bohemia Swarm Area P. Hrubcová et al. https://doi.org/10.1002/2015JB012548
- Tomographic imaging of the NW edge of the Hellenic volcanic arc A. Karakonstantis et al. https://doi.org/10.1007/s10950-019-09849-8
- New Velocity Structure of the Nový Kostel Earthquake-Swarm Region, West Bohemia, Determined by the Isometric Inversion J. Málek et al. https://doi.org/10.1007/s00024-023-03250-w
- The State of the Art in Studying the Deep Structure of the Earth’s Crust and Upper Mantle beneath the Baikal Rift from Seismological Data A. Seredkina https://doi.org/10.1134/S1069351321020117
- Detailed velocity ratio mapping during the aftershock sequence as a tool to monitor the fluid activity within the fault plane M. Bachura & T. Fischer https://doi.org/10.1016/j.epsl.2016.08.017
- New Research Perspectives in Light of Dense Cross-Border Experiments in West Bohemia and Vogtland Regions P. Büyükakpınar et al. https://doi.org/10.1007/s11200-026-00025-6
21 citations as recorded by crossref.
- Seismic tomography reveals a mid-crustal intrusive body, fluid pathways and their relation to the earthquake swarms in West Bohemia/Vogtland S. Mousavi et al. https://doi.org/10.1093/gji/ggv338
- Alteration as possible cause for transition from brittle failure to aseismic slip: the case of the NW-Bohemia / Vogtland earthquake swarm region J. Heinicke et al. https://doi.org/10.1016/j.jog.2019.01.010
- Kinematics of Crystal Growth in Single‐Seal Syntaxial Veins in Limestone ‐ A Phase‐Field Study M. Späth et al. https://doi.org/10.1029/2021JB022106
- Three-dimensional S-wave velocity model of the Bohemian Massif from Bayesian ambient noise tomography L. Valentová et al. https://doi.org/10.1016/j.tecto.2017.08.033
- Can hydroseismicity explain recurring earthquake swarms in NW-Bohemia? J. Heinicke et al. https://doi.org/10.1093/gji/ggx412
- ICDP drilling of the Eger Rift observatory: magmatic fluids driving the earthquake swarms and deep biosphere T. Fischer et al. https://doi.org/10.5194/sd-31-31-2022
- Tears, windows, and signature of transform margins on slabs. Images of the Cocos plate fragmentation beneath the Tehuantepec isthmus (Mexico) using Enhanced Seismic Models M. Calò https://doi.org/10.1016/j.epsl.2021.116788
- Clustering of 2008 West Bohemian seismic swarm mechanisms and its possible interpretation P. Kolar https://doi.org/10.13168/AGG.2018.0001
- Wadati method as a simple tool to study seismically active fault zones: a case study from the West-Bohemia/Vogtland region, central Europe O. Novotný et al. https://doi.org/10.1007/s11200-015-1206-1
- Event couple spectral ratio Q method for earthquake clusters: application to northwest Bohemia M. Kriegerowski et al. https://doi.org/10.5194/se-10-317-2019
- Anatomy of the Campi Flegrei caldera using Enhanced Seismic Tomography Models M. Calò & A. Tramelli https://doi.org/10.1038/s41598-018-34456-x
- Focal Mechanisms of West Bohemia, Central Europe, Earthquakes—End of May 2014: Evidence of Volume Changes D. Křížová & J. Málek https://doi.org/10.1785/0220200389
- Automated microseismic event location using Master-Event Waveform Stacking F. Grigoli et al. https://doi.org/10.1038/srep25744
- Geophysical characterization of the Cerro Machin geothermal area using three dimensional seismic and resistivity models J. Herrera & M. Calò https://doi.org/10.1016/j.geothermics.2025.103370
- CO2 degassing in the Hartoušov mofette area, western Eger Rift, imaged by CO2 mapping and geoelectrical and gravity surveys T. Nickschick et al. https://doi.org/10.1007/s00531-014-1140-4
- Shallow crustal discontinuities inferred from waveforms of microearthquakes: Method and application to KTB Drill Site and West Bohemia Swarm Area P. Hrubcová et al. https://doi.org/10.1002/2015JB012548
- Tomographic imaging of the NW edge of the Hellenic volcanic arc A. Karakonstantis et al. https://doi.org/10.1007/s10950-019-09849-8
- New Velocity Structure of the Nový Kostel Earthquake-Swarm Region, West Bohemia, Determined by the Isometric Inversion J. Málek et al. https://doi.org/10.1007/s00024-023-03250-w
- The State of the Art in Studying the Deep Structure of the Earth’s Crust and Upper Mantle beneath the Baikal Rift from Seismological Data A. Seredkina https://doi.org/10.1134/S1069351321020117
- Detailed velocity ratio mapping during the aftershock sequence as a tool to monitor the fluid activity within the fault plane M. Bachura & T. Fischer https://doi.org/10.1016/j.epsl.2016.08.017
- New Research Perspectives in Light of Dense Cross-Border Experiments in West Bohemia and Vogtland Regions P. Büyükakpınar et al. https://doi.org/10.1007/s11200-026-00025-6
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