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”

Evolution and Structure of the European Variscan Lithospheric Mantle

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F25%3A00642755" target="_blank" >RIV/67985831:_____/25:00642755 - isvavai.cz</a>

  • Result on the web

    <a href="https://pubs.geoscienceworld.org/msa/elements/article/21/6/408/720529/Evolution-and-Structure-of-the-European-Variscan" target="_blank" >https://pubs.geoscienceworld.org/msa/elements/article/21/6/408/720529/Evolution-and-Structure-of-the-European-Variscan</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.2138/gselements.21.6.408" target="_blank" >10.2138/gselements.21.6.408</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Evolution and Structure of the European Variscan Lithospheric Mantle

  • Original language description

    Tectonically emplaced peridotites and mantle xenoliths present complementary aspects of the evolution of the Variscan lithospheric mantle. The former have diverse origins and document complex histories of melt-rock reactions, exhumation along various pressure–temperature–time (P–T–t) paths, and emplacement into the crust, unravelling plate boundary evolution during Variscan subduction and collision. Mantle xenoliths exhumed by Cenozoic volcanism reveal ancient partial melting and mostly post-Variscan metasomatism episodes. Yet, their coarse-grained textures potentially record Variscan deformation. Dominantly belt-parallel fast seismic directions of the in situ Variscan lithospheric mantle may record flow normal to the convergence direction, but parallel to the boundaries of the Baltica and Avalonia blocks in central Europe, and to the main strike-slip faults and late extension in the Massif Central and Iberia.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10505 - Geology

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2025

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Elements

  • ISSN

    1811-5209

  • e-ISSN

    1811-5217

  • Volume of the periodical

    21

  • Issue of the periodical within the volume

    6

  • Country of publishing house

    CA - CANADA

  • Number of pages

    7

  • Pages from-to

    408-414

  • UT code for WoS article

    001663614900005

  • EID of the result in the Scopus database

    2-s2.0-105027138147