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Formation of elongated granite-migmatite domes as isostatic accommodation structures in collisional orogens

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F14%3A10283110" target="_blank" >RIV/00216208:11310/14:10283110 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985530:_____/14:00425801 RIV/00025798:_____/14:00000032

  • Result on the web

    <a href="http://dx.doi.org/10.1016/j.jog.2013.10.002" target="_blank" >http://dx.doi.org/10.1016/j.jog.2013.10.002</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.jog.2013.10.002" target="_blank" >10.1016/j.jog.2013.10.002</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Formation of elongated granite-migmatite domes as isostatic accommodation structures in collisional orogens

  • Original language description

    The mid-Carboniferous Pelhrimov core complex, Bohemian Massif, is a crustal-scale elongated granite-migmatite dome interpreted to have formed by gravity-driven diapiric upwelling of the metapelitic middle crust. The vertical diapiric flow is evidenced byoutward-dipping foliation and lineation patterns, deformation coeval with the widespread presence of melt, rapid exhumation of the dome center from depths corresponding to pressure of about 0.6 GPa to shallow levels (pressure less than 0.2 GPa) within 2M.y., and kinematic indicators of downward return flow of the mantling rocks. As compared to common diapirs, however, the Pelhrimov complex exhibits a more complicated inferred strain pattern with two perpendicular, irregularly alternating directions ofhorizontal extension in what is interpreted as the diapir head. Comparison of structural data from migmatites with anisotropy of magnetic susceptibility (AMS) data in granites also reveals that only final increments of strain are recorde

  • 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

    Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

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 Geodynamics

  • ISSN

    0264-3707

  • e-ISSN

  • Volume of the periodical

    73

  • Issue of the periodical within the volume

    leden

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    18

  • Pages from-to

    100-117

  • UT code for WoS article

    000336235900009

  • EID of the result in the Scopus database