Seismicity in the platform regions of Ukraine in the zones of anomalous electrical conductivity
It is established for the first time that there are several regions in Ukraine, in which the earthquakes occurring within platform territory are correlated to the anomalous conductive structures in the Earth’s crust and upper mantle. These regions are identified as (1) Donbass and the eastern part o...
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Veröffentlicht in: | Izvestiya. Physics of the solid earth 2013-05, Vol.49 (3), p.392-401 |
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creator | Kushnir, A. N. Kulik, S. N. Burakhovich, T. K. |
description | It is established for the first time that there are several regions in Ukraine, in which the earthquakes occurring within platform territory are correlated to the anomalous conductive structures in the Earth’s crust and upper mantle. These regions are identified as (1) Donbass and the eastern part of the Dnieper-Donetsk Depression (DDD); (2) eastern margin of the Ingulets-Krivoi Rog suture zone in the area of the Krivoi Rog-Kremenchug fault zone; (3) the western part of the Cis-Azov megablock; (4) the western boundary of the Ukrainian Shield and its slope; (5) North Dobruja and Pre-Dobrujan Depression. The reconstructed tree-dimensional (3D) geoelectrical models of the Earth’s crust and upper mantle feature anomalously low values of electric resistivity. The earthquake sources in the platform areas of Ukraine are localized above the top and in the upper parts of the crustal anomalies of electrical conductivity. |
doi_str_mv | 10.1134/S1069351313030087 |
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The reconstructed tree-dimensional (3D) geoelectrical models of the Earth’s crust and upper mantle feature anomalously low values of electric resistivity. The earthquake sources in the platform areas of Ukraine are localized above the top and in the upper parts of the crustal anomalies of electrical conductivity.</description><subject>Conductivity</subject><subject>Depression</subject><subject>Earth and Environmental Science</subject><subject>Earth crust</subject><subject>Earth Sciences</subject><subject>Earthquakes</subject><subject>Electrical conductivity</subject><subject>Electrical resistivity</subject><subject>Geophysics/Geodesy</subject><subject>Mantle</subject><subject>Mathematical models</subject><subject>Plate tectonics</subject><subject>Platforms</subject><subject>Resistivity</subject><subject>Seismic activity</subject><subject>Seismic phenomena</subject><subject>Seismology</subject><subject>Upper mantle</subject><issn>1069-3513</issn><issn>1555-6506</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNqFkU9PAyEQxYnRxFr9AN5IvHhZhWVh2aNp_Jc08VB7Jiw7W6m7UGFrUj-91GpiNMYThPm992YYhE4puaCUFZczSkTFOGWUEUaILPfQiHLOM8GJ2E_3VM629UN0FOOSkKJgVTVCagY29tbYYYOtw8MT4FWnh9aHHgdYWO8i9i2ePwdtHXwhb97Bx7t2vtedX0cMHZghWKM7bLxr1mawr8n0GB20uotw8nmO0fzm-nFyl00fbu8nV9NMF4QPmTF1K4xkOeNaciGhbXLSGgABsuK01lUjTC5rxiVoyhtdcyA0l7TQtakbwcbofOe7Cv5lDXFQvY0Guk47SO0pWpaE5TJPCf-i6cdSjhA8oWc_0KVfB5cGUZTxkoiSFjJRdEeZ4GMM0KpVsL0OG0WJ2m5H_dpO0uQ7TUysW0D45vyn6B3KfpGi</recordid><startdate>20130501</startdate><enddate>20130501</enddate><creator>Kushnir, A. 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Physics of the solid earth</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kushnir, A. N.</au><au>Kulik, S. N.</au><au>Burakhovich, T. K.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Seismicity in the platform regions of Ukraine in the zones of anomalous electrical conductivity</atitle><jtitle>Izvestiya. Physics of the solid earth</jtitle><stitle>Izv., Phys. Solid Earth</stitle><date>2013-05-01</date><risdate>2013</risdate><volume>49</volume><issue>3</issue><spage>392</spage><epage>401</epage><pages>392-401</pages><issn>1069-3513</issn><eissn>1555-6506</eissn><abstract>It is established for the first time that there are several regions in Ukraine, in which the earthquakes occurring within platform territory are correlated to the anomalous conductive structures in the Earth’s crust and upper mantle. These regions are identified as (1) Donbass and the eastern part of the Dnieper-Donetsk Depression (DDD); (2) eastern margin of the Ingulets-Krivoi Rog suture zone in the area of the Krivoi Rog-Kremenchug fault zone; (3) the western part of the Cis-Azov megablock; (4) the western boundary of the Ukrainian Shield and its slope; (5) North Dobruja and Pre-Dobrujan Depression. The reconstructed tree-dimensional (3D) geoelectrical models of the Earth’s crust and upper mantle feature anomalously low values of electric resistivity. The earthquake sources in the platform areas of Ukraine are localized above the top and in the upper parts of the crustal anomalies of electrical conductivity.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S1069351313030087</doi><tpages>10</tpages></addata></record> |
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subjects | Conductivity Depression Earth and Environmental Science Earth crust Earth Sciences Earthquakes Electrical conductivity Electrical resistivity Geophysics/Geodesy Mantle Mathematical models Plate tectonics Platforms Resistivity Seismic activity Seismic phenomena Seismology Upper mantle |
title | Seismicity in the platform regions of Ukraine in the zones of anomalous electrical conductivity |
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