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Intermediate granulite produced by transformation of eclogite at a felsic granulite contact, in Blanský les, Bohemian Massif

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F14%3A00000156" target="_blank" >RIV/00025798:_____/14:00000156 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11310/14:10218415

  • Result on the web

    <a href="http://onlinelibrary.wiley.com/doi/10.1111/jmg.12079/abstract" target="_blank" >http://onlinelibrary.wiley.com/doi/10.1111/jmg.12079/abstract</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1111/jmg.12079" target="_blank" >10.1111/jmg.12079</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Intermediate granulite produced by transformation of eclogite at a felsic granulite contact, in Blanský les, Bohemian Massif

  • Original language description

    Layers or bodies of intermediate granulite on scales from a centimetre to a hundred metres occur commonly within the felsic granulite massifs of the Bohemian Massif. Their origin is enigmatic in that they commonly have complex microstructures that are difficult to interpret, and therefore even the sequence of crystallization of minerals is uncertain. At Kleť, in the Blanský les massif, there is a revealing outcrop in a low-strain zone in which it is clear that intermediate granulite can form by the interaction of felsic granulite with eclogite. The eclogite, retains garnet from its eclogite heritage, the grains at least partially isolated from the matrix by a plagioclase corona. The original omphacite-dominated matrix of the eclogite now consists of recrystallized diopsidic clinopyroxene, orthopyroxene and plagioclase, with minor brown amphibole and quartz. The modification of the eclogite is dominated by the addition of just K2O and H2O, rather than all the elements that would be invo

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DB - Geology and mineralogy

  • OECD FORD branch

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • 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

  • Name of the periodical

    Journal of Metamorphic Geology

  • ISSN

    0263-4929

  • e-ISSN

  • Volume of the periodical

    32

  • Issue of the periodical within the volume

    4

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    23

  • Pages from-to

    347-370

  • UT code for WoS article

    000333540600024

  • EID of the result in the Scopus database