All

What are you looking for?

All
Projects
Results
Organizations

Quick search

  • Projects supported by TA ČR
  • Excellent projects
  • Projects with the highest public support
  • Current projects

Smart search

  • That is how I find a specific +word
  • That is how I leave the -word out of the results
  • “That is how I can find the whole phrase”

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

  • Czech description

Classification

  • Type

    C - Chapter in a specialist book

  • CEP classification

    DB - Geology and mineralogy

  • OECD FORD branch

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