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SEISMOLOGICAL ANALYSIS OF THE SWARM TYPE SEISMICITY IN THE REGION OF VELINGRAD, BULGARIA
Abstract
-he space-time distribution of earthquakes is of substantial importance for understanding the physics of the earthquake generation process. Earthquakes can be analyzed as a time series of events that result from the released strain in the earth's crust. The study of the space-time distribution of earthquakes using statistical methods reveals many of their characteristics. Sequences of seismic events affect both spatial and time distribution of earthquakes. It is necessary to know the statistical characteristics of the different seismic clusters and to reflect their impact in the general research related to seismicity. In the study, we analyze the swarm type sequence located in the vicinity of the town of Velingrad. The region is characterized with moderate seismic activity. Moreover, a reduced number of small earthquakes have also been registered in the recent past. About 30 events with magnitude in the range of 1.2?M?3.0 are recorded at Bulgarian seismological network in a time period of 10 days. The events are localized on and close to a defined fault structure. Most of the swarm events are with a magnitude in the range of 2.0-2.5. The earthquakes are located in the Earth-s crust at a depth up to 15 km. Rapid transition to background seismicity is observed after the generation of the strongest earthquakes in of the sequence.
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