Indications for a successively triggered rupture growth underlying the 2000 earthquake swarm in Vogtland/NW Bohemia
By Sebastian Hainzl, T. Fischer. 2002
183 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/76d29850b4d2edfee369d8f13f354d1a45df219f
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In Geophysics
- F. Finck
- Yosihiko Ogata
- Christian Ulrich Grosse
- D. Shelly
- David P. Hill
- William Ellsworth
- Sebastian Hainzl
- J. Kurz
Citations in the corpus
- Rate‐Dependent Incompleteness of Earthquake Catalogs (2016, background): “…(ETAS) model (Ogata, 1988; Zhuang et al., 2012) and to evaluate variations of statistical parameters such as the b-value (e.g., Imoto, 1991; Hainzl and Fischer, 2002; Mallika et al., 2013; Schurr et al., 2014; Huang and Beroza, 2015) or Omori c-value (e.g., Shcherbakov et al., 2004;…”
- Stress Drop and Stress Redistribution in Concrete Quantified Over Time by the b-value Analysis (2006, methodology): “The cumulative frequency–magnitude distribution was originally used in seismology to characterize earthquake populations [1].”
- Detecting fluid signals in seismicity data through statistical earthquake modeling (2005, methodology): “[7] From previous investigations of this earthquake swarm [Hainzl and Fischer, 2002; Fischer, 2003], it is known that (1) all the earthquakes occur approximately on the same fault plane; (2) the spatial spreading of the swarm activity scales with the cumulative seismic moment release according to…”
- The 2012 Brawley swarm triggered by injection-induced aseismic slip (2015, background): “9b and 9c), are similar to that observed elsewhere in naturally occurring swarms (Cappa et al., 2009; Hainzl and Fischer, 2002; Vidale and Shearer, 2006).”
- Fluid‐faulting evolution in high definition: Connecting fault structure and frequency‐magnitude variations during the 2014 Long Valley Caldera, California, earthquake swarm (2016, background): “Studies that have looked at the relationship between ML and seismic moment in detail have supported this, for example, finding equivalent c values for ML of 5/6 (for ML 1.5–3.5 events in California [Bakun, 1984]) or 0.95 (ML 0.3–3.0 events in Western Bohemia [Hainzl and Fischer, 2002]), both signifi”