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Statements

Subject Item
n2:RIV%2F67985831%3A_____%2F12%3A00382559%21RIV13-AV0-67985831
rdf:type
n13:Vysledek skos:Concept
rdfs:seeAlso
http://www.geologicacarpathica.sk/src/main.php
dcterms:description
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° for reversed polarity (Pleistocene); or 345 to 350° and around 62° 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 Bruntál 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 (4.3–3.3 Ma), Břidličná Volcano, was simultaneously active with the Lutynia Volcano (Poland) which produced the Zálesí lava relic (normal polarity). Three other volcanoes of the volcanic field are younger and reversely polarized. The Velký Roudný Volcano was active during the Gelasian (2.6–2.1 Ma) and possibly could have been reactivated during the youngest (Calabrian, 1.8–1.1 Ma) phase which gave birth to the Venušina sopka and Uhlířský vrch volcanoes. The reliability of all available K-Ar data was evaluated using a multidisciplinary approach. 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° for reversed polarity (Pleistocene); or 345 to 350° and around 62° 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 Bruntál 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 (4.3–3.3 Ma), Břidličná Volcano, was simultaneously active with the Lutynia Volcano (Poland) which produced the Zálesí lava relic (normal polarity). Three other volcanoes of the volcanic field are younger and reversely polarized. The Velký Roudný Volcano was active during the Gelasian (2.6–2.1 Ma) and possibly could have been reactivated during the youngest (Calabrian, 1.8–1.1 Ma) phase which gave birth to the Venušina sopka and Uhlířský vrch volcanoes. The reliability of all available K-Ar data was evaluated using a multidisciplinary approach.
dcterms:title
Chronological implications of the paleomagnetic record of the Late Cenozoic volcanic activity along the Moravia-Silesia border (NE Bohemian Massif) Chronological implications of the paleomagnetic record of the Late Cenozoic volcanic activity along the Moravia-Silesia border (NE Bohemian Massif)
skos:prefLabel
Chronological implications of the paleomagnetic record of the Late Cenozoic volcanic activity along the Moravia-Silesia border (NE Bohemian Massif) Chronological implications of the paleomagnetic record of the Late Cenozoic volcanic activity along the Moravia-Silesia border (NE Bohemian Massif)
skos:notation
RIV/67985831:_____/12:00382559!RIV13-AV0-67985831
n13:predkladatel
n20:ico%3A67985831
n3:aktivita
n8:Z n8:P n8:I
n3:aktivity
I, P(GAP210/10/2351), P(IAA300130612), Z(AV0Z30130516)
n3:cisloPeriodika
5
n3:dodaniDat
n14:2013
n3:domaciTvurceVysledku
n9:8523495 n9:4952472 n9:1361074 n9:6180159 n9:9827625
n3:druhVysledku
n10:J
n3:duvernostUdaju
n6:S
n3:entitaPredkladatele
n19:predkladatel
n3:idSjednocenehoVysledku
127163
n3:idVysledku
RIV/67985831:_____/12:00382559
n3:jazykVysledku
n18:eng
n3:klicovaSlova
Plio-Pleistocene basalts; paleomagnetism; magnetostratigraphy; volcanology; K/Ar dating,; airborne magnetometry and gravimetry; Moravia and Silesia
n3:klicoveSlovo
n5:Moravia%20and%20Silesia n5:airborne%20magnetometry%20and%20gravimetry n5:volcanology n5:Plio-Pleistocene%20basalts n5:magnetostratigraphy n5:K%2FAr%20dating n5:paleomagnetism
n3:kodStatuVydavatele
SK - Slovenská republika
n3:kontrolniKodProRIV
[FA5767E106D3]
n3:nazevZdroje
Geologica Carpathica
n3:obor
n17:DE
n3:pocetDomacichTvurcuVysledku
5
n3:pocetTvurcuVysledku
7
n3:projekt
n15:GAP210%2F10%2F2351 n15:IAA300130612
n3:rokUplatneniVysledku
n14:2012
n3:svazekPeriodika
63
n3:tvurceVysledku
Skácelová, Z. Cajz, Vladimír Schnabl, Petr Pécskay, Z. Šlechta, Stanislav Venhodová, Daniela Čížková, Kristýna
n3:wos
000311260600006
n3:zamer
n4:AV0Z30130516
s:issn
1335-0552
s:numberOfPages
13