Permian clockwise rotations of the Ebro and Corso-Sardinian blocks during Iberian?Armorican oroclinal bending: Preliminary paleomagnetic data from the Catalan Coastal Range (NE Spain)

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F15%3A00000281" target="_blank" >RIV/00025798:_____/15:00000281 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.1016/j.tecto.2015.07.002" target="_blank" >http://dx.doi.org/10.1016/j.tecto.2015.07.002</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.tecto.2015.07.002" target="_blank" >10.1016/j.tecto.2015.07.002</a>

Result language
angličtina
Original language name
Permian clockwise rotations of the Ebro and Corso-Sardinian blocks during Iberian?Armorican oroclinal bending: Preliminary paleomagnetic data from the Catalan Coastal Range (NE Spain)
Original language description
Paleomagnetic investigations of Early Permian and Triassic magmatic rocks from Catalan Coastal Ranges provide three magnetic directions which are interpreted as primary magnetizations and partly as overprints. The succession of magnetic directions is interpreted in terms of a succession of large-scale clockwise rotations, which bring the whole assembly of Pyrenees, Catalonia, Corsica-Sardinia and Maures-Esterel massifs from the southeast of the Massif Central to the west during Permian. This major movement is associated with clockwise rotation of northern limb of the Iberian orocline during Latest Carboniferous and Early Permian (~ 305-290 Ma). Subsequently, Permian large-scale dextral transtensional-extensional shearing operated along Aquitanian ShearBelt between the Massif Central in the northeast and the Iberian Variscan massifs in the southwest. The latest phase of the rotation in the Late Permian-Early Triassic is associated with alkaline magmatism probably linked to Neo-Tethys o
Czech name
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Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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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)

Publication year
2015
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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