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- W3173022084 abstract "<p>The East Baltic region (EBR), located on the ancient Precambrian East European Craton, is characterized by low seismic and deformational activity. The EBR is located at a distance of about 2000 km from the divergent zone in the North Atlantic and from the convergent zone in the Mediterranean Sea.</p><p>Nevertheless, historical and modern earthquakes have occurred in the EBR. Historical earthquakes occurred in 1616 (<em>Bauska</em>, Latvia, VI), 1670 (<em>P&#228;rnu</em>, Estonia, VI), 1821 (<em>Koknese</em>, Latvia, VI), 1823 (<em>V&#245;rtsj&#228;rv</em>, Estonia, VI), 1857 (<em>Irbe</em>, Latvia, VI), 1896 (<em>Jelgava</em>, Latvia, V), and modern earthquakes occurred on 10/25/1976 (<em>Osmussaar</em>, Estonia, M 4.7), 09/21/2004 (<em>Kaliningrad</em> region, Russia, Mw 5.2).</p><p>The study of slow (tectonic creep) and fast (earthquakes) deformations is practical importance in EBR for safety of energy facilities - <em>Plavinas</em> HPP, <em>Baltic</em> (Kaliningrad region of Russia) NPP and <em>Ostrovets</em> (Belarus) NPP.</p><p>In the central part of the territory of Latvia, signs of geodynamic activity of the Earth's crust have been identified. A characteristic feature is the trans-regional <em>Olaine-In&#269;ukalns</em> tectonic fault, which crosses the Riga agglomeration. The fault is traced in the <em>Caledonian</em> structural complex.</p><p>Previous studies on seismic hazard assessment in Latvia (Safronovs & Nikulins, 1999; Nikulins, 2011) were based on combination of seismic, geophysical, geodetic and geological data. These studies made it possible to assess the seismotectonic potential of the Earth's crust, parameters of seismogenic zones and to state a very low seismic activity.</p><p>A sparse seismic network and poor seismic-geological conditions affect the effectiveness of seismological monitoring in EBR. To understand of driving mechanisms for earthquakes, results of remote sensing (<em>Persistent Scatterer Interferometry - PSI</em>) of surface (1992 - 2000), studies of radon anomalies (2014), and macroseismic data (2010) were used.</p><p><em>PSI</em> method made it possible to reveal the anomalous vertical velocity (25.4 mm/year) of opposite sides of fault, adjacent to the <em>Olaine-In&#269;ukalns</em> fault in the southwest of Riga. The average vertical velocity does not exceed 1.03 mm/year. The study of the radon field in northeast of the <em>Olaine-In&#269;ukalns</em> fault revealed an intense (140000 Bq/m<sup>3</sup>) radon anomaly (Nikulins, 2014).</p><p>In addition, on 22.11.2010, population of Riga and its environs felt shaking. Mechanism of the <em>Olaine-In&#269;ukalns</em> fault is predominately <em>thrust faulting</em> with a <em>strike-slip</em> component, whereas mechanisms of most other faults in Latvia are <em>normal faulting</em> type.</p><p>These signs indicate the activation of the <em>Olaine-In&#269;ukalns</em> tectonic fault. Thus, on the EBR, under conditions of slow deformation of the Earth's crust, a comprehensive analysis of various geological, geophysical and deformation parameters has justified itself.<br><br></p><p>Literature</p><p>Nikulins V., 2014. <em>Geodynamic Hazard Factors of Latvia: Experimental data and Computational Analysis</em>. Baltic Journal of Modern Computing, 7 (1), 151 &#8211; 170.</p><p>Safronovs O.N., Nikulins V.G., 1999. <em>General seismic zoning of Latvia</em>. Latvian geology news, 6, 30 - 35. (In Latvian).</p><p>Nikulin V., 2011. <em>Assessment of the seismic hazard in Latvia. Version of 2007 year</em>. RTU science articles. Materials Science and Applied Chemistry, 1 (24), 110 &#8211; 115.</p>" @default.
- W3173022084 created "2021-06-22" @default.
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- W3173022084 date "2021-03-04" @default.
- W3173022084 modified "2023-09-24" @default.
- W3173022084 title "An integrated approach to assessing the geodynamic activity of the Earth's crust in the low seismic East Baltic region" @default.
- W3173022084 doi "https://doi.org/10.5194/egusphere-egu21-8877" @default.
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