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P?T?t?d evolution of orogenic middle crust of the Roc de Frausa Massif (Eastern Pyrenees): A result of horizontal crustal flow and Carboniferous doming?

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F15%3A00000183" target="_blank" >RIV/00025798:_____/15:00000183 - isvavai.cz</a>

  • Result on the web

    <a href="http://onlinelibrary.wiley.com/doi/10.1111/jmg.12120/abstract" target="_blank" >http://onlinelibrary.wiley.com/doi/10.1111/jmg.12120/abstract</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1111/jmg.12120" target="_blank" >10.1111/jmg.12120</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    P?T?t?d evolution of orogenic middle crust of the Roc de Frausa Massif (Eastern Pyrenees): A result of horizontal crustal flow and Carboniferous doming?

  • Original language description

    In the Roc de Frausa Massif in the Eastern Pyrenees, the pre-Variscan lithological succession is the Upper, Intermediate and Lower series by two orthogneiss sheets and intruded by Variscan igneous rocks. Two phases of Variscan deformation. D1 are markedby flat-lying foliation (S1) that affects the whole crustal section, D2 structures are characterized by tight upright folds facing to the NW with steep NE?SW axial planes, D2 leads to an almost complete transposition into a sub-vertical foliation (S2) inthe high-grade metamorphic domain. In the Upper series, and-sill grew during the S1 indicating heating from 580 to 640°C associated with an increase in pressure. Static growth of cordierite points to post-D1 decompression. In the Intermediate series, asill?bi?mu-bearing assemblage parallel to the S1 is statically overgrown by crd-ksp. This points to ~1 kbar of post-D1 decompression at 630?650°C. The Intermediate series intruded by a gabbro?diorite has a aureole where, the migmatitic S1

  • 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

    2015

  • 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

    33

  • Issue of the periodical within the volume

    3

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    22

  • Pages from-to

    273-294

  • UT code for WoS article

    000351210400003

  • EID of the result in the Scopus database