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
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F14%3A00000103" target="_blank" >RIV/00025798:_____/14:00000103 - isvavai.cz</a>
Result on the web
<a href="http://sp.lyellcollection.org/content/405/1/333.abstract" target="_blank" >http://sp.lyellcollection.org/content/405/1/333.abstract</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1144/SP405.10" target="_blank" >10.1144/SP405.10</a>
Alternative languages
Result language
angličtina
Original language name
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
Original language 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
Czech name
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Czech description
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Classification
Type
C - Chapter in a specialist book
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Result continuities
Project
<a href="/en/project/LK11202" target="_blank" >LK11202: The role of Paleozoic accretionary and collisanal orogens on the formation and growth of continental crust</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2014
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Book/collection name
The Variscan orogeny: extent, timescale and the formation of the European crust
ISBN
978-1-86239-658-6
Number of pages of the result
28
Pages from-to
333-361
Number of pages of the book
406
Publisher name
The Geological Society of London
Place of publication
London
UT code for WoS chapter
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