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U?Pb zircon provenance of Moldanubian metasediments in the Bohemian Massif

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F14%3A00424604" target="_blank" >RIV/67985831:_____/14:00424604 - isvavai.cz</a>

  • Alternative codes found

    RIV/00025798:_____/14:00000026

  • Result on the web

    <a href="http://dx.doi.org/10.1144/jgs2013-059" target="_blank" >http://dx.doi.org/10.1144/jgs2013-059</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1144/jgs2013-059" target="_blank" >10.1144/jgs2013-059</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    U?Pb zircon provenance of Moldanubian metasediments in the Bohemian Massif

  • Original language description

    Detrital zircon U?Pb age data from the Moldanubian part of the Bohemian Massif obtained by laser ablation inductively coupled plasma mass spectrometry show variations between the lithotectonic units and point to their formation in spatially close but separated basins that were supplied by detritus from somewhat different source areas, possibly over different periods of time. The youngest detrital zircon component in metasediments of the Monotonous and Varied Units is Early Ordovician and Mid- to Late Devonian in age, respectively, suggesting their deposition in Palaeozoic times. Reliable interpretation of the Mid- to Late Devonian zircons recovered from metasediments of the Gföhl Unit is precluded by their high metamorphic grade and presence of anatectic melt. The Early Carboniferous zircons from the Gföhl Unit are interpreted as being of metamorphic origin. Comparison of detrital zircon age spectra from the Moldanubian, Teplá? Barrandian and Moravo-Silesian metasediments suggests that

  • Czech name

  • Czech description

Classification

  • Type

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

  • CEP classification

    DD - Geochemistry

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GAP210%2F11%2F1904" target="_blank" >GAP210/11/1904: Deciphering the pre-convergence history of crustal domains in deeply eroded orogenic belts from detrital zircon populations</a><br>

  • Continuities

    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 the Geological Society

  • ISSN

    0016-7649

  • e-ISSN

  • Volume of the periodical

    171

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    13

  • Pages from-to

    83-95

  • UT code for WoS article

    000329924200009

  • EID of the result in the Scopus database