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Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F14%3A00000103%21RIV15-MSM-00025798
rdf:type
skos:Concept n12:Vysledek
rdfs:seeAlso
http://sp.lyellcollection.org/content/405/1/333.abstract
dcterms:description
Palaeomagnetic investigations of the Corso-Sardinian block and Maures–Estérel show that there has been a change in their magnetic orientation during the Late Carboniferous–Early Permian period (305–280 Ma). This trend is interpreted in terms of a large-scale 90° clockwise rotation of the southern branch of the Variscan belt that matches the successive change in shortening directions revealed by structural geology. The evidence is based on existing structural studies of the fabrics of syntectonically emplaced granitoids partly based on the anisotropy of magnetic susceptibility, combined with a large database of isotopic ages. The chronological match between the palaeomagnetic and tectonic datasets is interpreted here as a result of large-scale dextral wrench movements in the lithosphere between the Gondwana and Laurussia supercontinents. This wrench deformation is regarded as a sequel to the dextral rotation of the northern branch of the Variscan belt during 330–315 Ma which terminated in frontal collision with Avalonia. The continuation of movement in the southern Variscan realm was due to shearing along the southern margin of the Avalonian block. An additional clockwise rotation is inferred to have taken place during the Triassic period. The age of this motion remains to be determined. Palaeomagnetic investigations of the Corso-Sardinian block and Maures–Estérel show that there has been a change in their magnetic orientation during the Late Carboniferous–Early Permian period (305–280 Ma). This trend is interpreted in terms of a large-scale 90° clockwise rotation of the southern branch of the Variscan belt that matches the successive change in shortening directions revealed by structural geology. The evidence is based on existing structural studies of the fabrics of syntectonically emplaced granitoids partly based on the anisotropy of magnetic susceptibility, combined with a large database of isotopic ages. The chronological match between the palaeomagnetic and tectonic datasets is interpreted here as a result of large-scale dextral wrench movements in the lithosphere between the Gondwana and Laurussia supercontinents. This wrench deformation is regarded as a sequel to the dextral rotation of the northern branch of the Variscan belt during 330–315 Ma which terminated in frontal collision with Avalonia. The continuation of movement in the southern Variscan realm was due to shearing along the southern margin of the Avalonian block. An additional clockwise rotation is inferred to have taken place during the Triassic period. The age of this motion remains to be determined.
dcterms:title
Early Permian 90° clockwise rotation of the Maures–Estérel–Corsica–Sardinia block confirmed by new palaeomagnetic data and followed by a Triassic 60° clockwise rotation Early Permian 90° clockwise rotation of the Maures–Estérel–Corsica–Sardinia block confirmed by new palaeomagnetic data and followed by a Triassic 60° clockwise rotation
skos:prefLabel
Early Permian 90° clockwise rotation of the Maures–Estérel–Corsica–Sardinia block confirmed by new palaeomagnetic data and followed by a Triassic 60° clockwise rotation Early Permian 90° clockwise rotation of the Maures–Estérel–Corsica–Sardinia block confirmed by new palaeomagnetic data and followed by a Triassic 60° clockwise rotation
skos:notation
RIV/00025798:_____/14:00000103!RIV15-MSM-00025798
n3:aktivita
n20:P
n3:aktivity
P(LK11202)
n3:dodaniDat
n13:2015
n3:domaciTvurceVysledku
n10:2354691
n3:druhVysledku
n16:C
n3:duvernostUdaju
n7:S
n3:entitaPredkladatele
n8:predkladatel
n3:idSjednocenehoVysledku
12815
n3:idVysledku
RIV/00025798:_____/14:00000103
n3:jazykVysledku
n14:eng
n3:klicovaSlova
Variscan orogeny, paleomagnetism
n3:klicoveSlovo
n4:Variscan%20orogeny n4:paleomagnetism
n3:kontrolniKodProRIV
[3CD0069BF392]
n3:mistoVydani
London
n3:nazevEdiceCisloSvazku
Geological Society, London, Special Publications, 405
n3:nazevZdroje
The Variscan orogeny: extent, timescale and the formation of the European crust
n3:obor
n18:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetStranKnihy
406
n3:pocetTvurcuVysledku
5
n3:projekt
n9:LK11202
n3:rokUplatneniVysledku
n13:2014
n3:tvurceVysledku
Edel, Jean-Bernard Oggiano, Giacomo Schulmann, Karel Rossi, Phillipe Casini, Leonardo
s:numberOfPages
28
n15:doi
10.1144/SP405.10
n11:hasPublisher
The Geological Society of London
n17:isbn
978-1-86239-658-6