CARPATHIANS
Author:
Verbitskii S.1, Pronishin R.2, Verbitskii Iu.1, Chuba M.1, Keleman I.1, Stets'kiv A.1, Stepanenko N.3, Iliesh I.3, Alekseev I.3, Simonova N.3
Affiliation:
1. The Division of Carpathian Regions Seismicity of the Institute of Geophysics of the National Academy of Sciences of Ukraine, Lviv, Ukraine 2. The Division of Carpathian Regions Seismicity of the Institute of Geophysics of the National Academy of Sciences of Ukraine, Lviv 3. Institute of Geology and Seismology, Moldova Academy of Sciences, Kishinev, Republic of Moldova
Abstract
The seismic observations in the Carpathian region in 2013, which were conducted, as before, by two organizations from two states: in Ukraine, by the seismicity department of the Carpathian region of the Institute of Geophysics of the National Academy of Sciences of Ukraine, and in Moldova by the seismology laboratory of the Institute of Geology and Seismology of the Academy of Sciences of Moldova are described. There were 19 digital stations with a processing center in Lviv, Ukraine, and 6 stations with a center in Chisinau, Moldova. Various programs, local hodographs, and magnitudes were used. The consolidated catalog of earthquakes is created in Lviv. The map of epicenters and the table of the distribution of earthquakes of differ-ent classes by regions are given. The total number of earthquakes in 2013 was N=98 in the range of КР=5.7–14.1 and the depth interval of hypocenters h=1–150 km with total seismic energy Е=1.331014 J. Of these, 19 earthquakes with depths h=80–160 km is located in the Vrancea zone. Two maximum earth-quakes with КР=14.1 and КР=12.3 were recorded on October 6 and 15 in the Vrancea mountains with h=139.8 and 140.9 km. In Forecarpathians and Transcarpathia all earthquakes are weaker. The most significant event in Transcarpathia was the earthquake on April 4, 2013, with КР=8.4 in the area of «Nizhnее Selishche» seismic station. The earthquake source is located in the earth's crust at a depth of h=1.7 km. The earthquake was felt by the population of the Village Nizhnее Selishche with an intensity I=3–4. In general, in all seismic active zones of the Carpathians in 2013, there was a slight increase in the level of seismicity compared with that in 2012.
Publisher
Geophysical Survey of the Russian Academy of Sciences - GS RAS
Reference36 articles.
1. 1. Verbitskii, S.T., Pronishin, R.S., Stasiuk, A.F., Chuba, M.V., Verbitskii, Iu.T., Keleman, I.N., Stepa-nenko, N.Ia., Iliesh, I.I., Simonova, N.A., & Alekseev, I.V. (2018). Carpathians. Zemletriaseniia Severnoi Evrazii [Earthquakes in Northern Eurasia], 21 (2012), 40–48. (In Russ.). 2. 2. Verbitskii, S.T., Stasiuk, A.F., Chuba, M.V., Pronishin, R.S., Keleman, I.M., Garandzha, I.A., & Verbit-skii, Iu.T. (2014). [Carpathians]. In Zemletriaseniia Severnoi Evrazii, 2008 god [Earthquakes in Northern Eurasia, 2008] (pp. 60–66). Obninsk, Russia: GS RAS Publ. (In Russ.). 3. 3. Iliesh, I.I. (2008). [Seismic network of the Republic of Moldova: state and prospects]. In Seismichnost' Severnoi Evrazii. Materialy Mezhdunarodnoi konferentsii [Seismicity of Northern Eurasia. Proceeding of the International Conference] (pp. 87–92). Obninsk, Russia: GS RAS Publ. (In Russ.). 4. 4. Pronishin, R.S., Stasiuk, A.F., Chuba, M.V., Simonova, N.A., & Stepanenko, N.Ia. (2006). [Carpathians]. In Zemletriaseniia Severnoi Evrazii, 2000 god [Earthquakes in Northern Eurasia, 2000] (pp. 51–57). Obninsk, Russia: GS RAS Publ. (In Russ.). 5. 5. Pronishin, R.S., Stasiuk, A.F., Chuba, M.V., Garandzha, I.A., Keleman, I.M., Stepanenko, N.Ia., Alekseev, I.V., & Simonova, N.A. (2008). [Carpathians]. In Zemletriaseniia Severnoi Evrazii, 2002 god [Earthquakes in Northern Eurasia, 2000] (pp. 63–72). Obninsk, Russia: GS RAS Publ. (In Russ.).
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