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Statements

Subject Item
n2:RIV%2F67985831%3A_____%2F11%3A00368273%21RIV12-AV0-67985831
rdf:type
skos:Concept n19:Vysledek
rdfs:seeAlso
http://gq.pgi.gov.pl/gq/article/view/7602/pdf_23
dcterms:description
In Devonian carbonates of the Holy Cross Mountains (HCM) are documented the record of three individual episodes of remagnetisation. The fold test performed within map-scale folds from central part of the HCM documented early synfolding origin of the Viséan component and postfolding nature of the Early Permian and Permo/Triassic overprints. The results confirmed that the westernmost parts of the HCM were rotated clockwise after the Early Permian. Paleomagnetic studies of this zone documented shape modifications in part of the large map-scale folds as well as some of smaller meso-scale folds. Such a tectonic overprint occurred after the Early Permian, most probably in the course of Late Variscan deformations. Further results indicate that the studied N-S trending dextral strike-slip faults were active between the Early Permian and the Permo/Triassic period. Overlying breccia that covers discordantly deformed Devonian strata was formed after the Early Permian. In Devonian carbonates of the Holy Cross Mountains (HCM) are documented the record of three individual episodes of remagnetisation. The fold test performed within map-scale folds from central part of the HCM documented early synfolding origin of the Viséan component and postfolding nature of the Early Permian and Permo/Triassic overprints. The results confirmed that the westernmost parts of the HCM were rotated clockwise after the Early Permian. Paleomagnetic studies of this zone documented shape modifications in part of the large map-scale folds as well as some of smaller meso-scale folds. Such a tectonic overprint occurred after the Early Permian, most probably in the course of Late Variscan deformations. Further results indicate that the studied N-S trending dextral strike-slip faults were active between the Early Permian and the Permo/Triassic period. Overlying breccia that covers discordantly deformed Devonian strata was formed after the Early Permian.
dcterms:title
Palaeomagnetic age constraints on folding and faulting events in devonian carbonates of the Kielce Fold Zone southern Holy Cross Mountains, Central Poland) Palaeomagnetic age constraints on folding and faulting events in devonian carbonates of the Kielce Fold Zone southern Holy Cross Mountains, Central Poland)
skos:prefLabel
Palaeomagnetic age constraints on folding and faulting events in devonian carbonates of the Kielce Fold Zone southern Holy Cross Mountains, Central Poland) Palaeomagnetic age constraints on folding and faulting events in devonian carbonates of the Kielce Fold Zone southern Holy Cross Mountains, Central Poland)
skos:notation
RIV/67985831:_____/11:00368273!RIV12-AV0-67985831
n19:predkladatel
n20:ico%3A67985831
n3:aktivita
n14:Z n14:P
n3:aktivity
P(GAP210/10/2351), Z(AV0Z30130516)
n3:cisloPeriodika
3
n3:dodaniDat
n9:2012
n3:domaciTvurceVysledku
n13:1361074
n3:druhVysledku
n16:J
n3:duvernostUdaju
n10:S
n3:entitaPredkladatele
n7:predkladatel
n3:idSjednocenehoVysledku
219403
n3:idVysledku
RIV/67985831:_____/11:00368273
n3:jazykVysledku
n17:eng
n3:klicovaSlova
paleomagnetic components; remagnetization; tectonics
n3:klicoveSlovo
n4:remagnetization n4:paleomagnetic%20components n4:tectonics
n3:kodStatuVydavatele
PL - Polská republika
n3:kontrolniKodProRIV
[A982C05CF911]
n3:nazevZdroje
Geological Quarterly
n3:obor
n11:DE
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
4
n3:projekt
n15:GAP210%2F10%2F2351
n3:rokUplatneniVysledku
n9:2011
n3:svazekPeriodika
55
n3:tvurceVysledku
Szaniawski, R. Grabowski, J. Schnabl, Petr Konon, A.
n3:wos
000296999800004
n3:zamer
n12:AV0Z30130516
s:issn
1641-7291
s:numberOfPages
12