"Sk\u00E1celov\u00E1, Z." . . . . "13"^^ . . . . . "http://www.geologicacarpathica.sk/src/main.php" . . "Chronological implications of the paleomagnetic record of the Late Cenozoic volcanic activity along the Moravia-Silesia border (NE Bohemian Massif)" . "This paper presents the results of a paleomagnetic study carried out on Plio-Pleistocene Cenozoic basalts from the NE part of the Bohemian Massif. Paleomagnetic data were supplemented by 27 newly obtained K/Ar age determinations. Lavas and volcaniclastics of 6 volcanoes were sampled. Declination and Inclination values of paleomagnetic vector vary in the spans of 130 to 174 and -85 to -68\u00B0 for reversed polarity (Pleistocene); or 345 to 350\u00B0 and around 62\u00B0 for normal polarity (Pliocene). Volcanological evaluation and compilation of older geophysical data from field survey served as the basis for the interpretation of these results. The Pleistocene volcanic stage consists of two volcanic phases, fairly closely spaced in time. Four volcanoes constitute the Brunt\u00E1l Volcanic Field; two others are located 20 km to the E and 65 km to the NW, respectively. The volcanoes are defined as monogenetic ones, producing scoria cones and lavas. Exceptionally, the largest volcano shows a possibility of remobilization during the youngest volcanic phase, suggested by paleomagnetic properties. The oldest one (4.3\u20133.3 Ma), B\u0159idli\u010Dn\u00E1 Volcano, was simultaneously active with the Lutynia Volcano (Poland) which produced the Z\u00E1les\u00ED lava relic (normal polarity). Three other volcanoes of the volcanic field are younger and reversely polarized. The Velk\u00FD Roudn\u00FD Volcano was active during the Gelasian (2.6\u20132.1 Ma) and possibly could have been reactivated during the youngest (Calabrian, 1.8\u20131.1 Ma) phase which gave birth to the Venu\u0161ina sopka and Uhl\u00ED\u0159sk\u00FD vrch volcanoes. The reliability of all available K-Ar data was evaluated using a multidisciplinary approach." . . "Cajz, Vladim\u00EDr" . "Plio-Pleistocene basalts; paleomagnetism; magnetostratigraphy; volcanology; K/Ar dating,; airborne magnetometry and gravimetry; Moravia and Silesia"@en . . . . . "Chronological implications of the paleomagnetic record of the Late Cenozoic volcanic activity along the Moravia-Silesia border (NE Bohemian Massif)"@en . . . "RIV/67985831:_____/12:00382559!RIV13-AV0-67985831" . "Schnabl, Petr" . . . . . "RIV/67985831:_____/12:00382559" . . . . "P\u00E9cskay, Z." . "[FA5767E106D3]" . "63" . "Chronological implications of the paleomagnetic record of the Late Cenozoic volcanic activity along the Moravia-Silesia border (NE Bohemian Massif)" . "\u0160lechta, Stanislav" . . "I, P(GAP210/10/2351), P(IAA300130612), Z(AV0Z30130516)" . "Venhodov\u00E1, Daniela" . "Geologica Carpathica" . "1335-0552" . . "5"^^ . "Chronological implications of the paleomagnetic record of the Late Cenozoic volcanic activity along the Moravia-Silesia border (NE Bohemian Massif)"@en . "This paper presents the results of a paleomagnetic study carried out on Plio-Pleistocene Cenozoic basalts from the NE part of the Bohemian Massif. Paleomagnetic data were supplemented by 27 newly obtained K/Ar age determinations. Lavas and volcaniclastics of 6 volcanoes were sampled. Declination and Inclination values of paleomagnetic vector vary in the spans of 130 to 174 and -85 to -68\u00B0 for reversed polarity (Pleistocene); or 345 to 350\u00B0 and around 62\u00B0 for normal polarity (Pliocene). Volcanological evaluation and compilation of older geophysical data from field survey served as the basis for the interpretation of these results. The Pleistocene volcanic stage consists of two volcanic phases, fairly closely spaced in time. Four volcanoes constitute the Brunt\u00E1l Volcanic Field; two others are located 20 km to the E and 65 km to the NW, respectively. The volcanoes are defined as monogenetic ones, producing scoria cones and lavas. Exceptionally, the largest volcano shows a possibility of remobilization during the youngest volcanic phase, suggested by paleomagnetic properties. The oldest one (4.3\u20133.3 Ma), B\u0159idli\u010Dn\u00E1 Volcano, was simultaneously active with the Lutynia Volcano (Poland) which produced the Z\u00E1les\u00ED lava relic (normal polarity). Three other volcanoes of the volcanic field are younger and reversely polarized. The Velk\u00FD Roudn\u00FD Volcano was active during the Gelasian (2.6\u20132.1 Ma) and possibly could have been reactivated during the youngest (Calabrian, 1.8\u20131.1 Ma) phase which gave birth to the Venu\u0161ina sopka and Uhl\u00ED\u0159sk\u00FD vrch volcanoes. The reliability of all available K-Ar data was evaluated using a multidisciplinary approach."@en . "127163" . "000311260600006" . . "5" . . "7"^^ . . "SK - Slovensk\u00E1 republika" . . "\u010C\u00ED\u017Ekov\u00E1, Krist\u00FDna" .