Record details

    Kalium-argonové datování bazaltové žíly ze Želešic (brněnský masiv) (24-34 Ivančice)
Statement of responsibility
    Antonín Přichystal
Other titles
    K-Ar determination of a basaltic dike from Želešice (Brno massif)
    Přichystal, Antonín, 1950-
Source title - serial
    Geologické výzkumy na Moravě a ve Slezsku
    Roč. 6
    s. 120-121
    7 bibl.
    Anglické resumé
    Zkr. název ser.: Geol. Výzk. Mor. Slez. v Roce 1998.
Subject group
    brněnský masiv
    datování K/Ar
Geographical name
    Lhota Rapotina (Blansko)
    Želešice (Brno-venkov)
Abstract (in english)
   The Brno massif has a characteristic two-part structure formed by eatsern and western granotoid sectors of Upper Proterozoic age. Relatively narrow (2-8 km) so called metabasite zone built of two belts (metadiorite belt on the west and metabasalte one on the east) is situated between granitoid parts. The author sampled a basaltic dike that together with a stock of rhyolite penetrates deformed and metamorphosed basic and ultrabasic rocks of the western metadiorite belt in the abandoned Old quarry at Želešice (8km south of Brno). The basaltic dike was analysed by K-Ar method in the Laboratory of Isotopic Geology, Geological Survey of Slovakia, Bratislava and it yielded the following data: 434 8 My (by isotopic dilution) and 438 16My (volumetrically).
   Comparing to the latest geological time scale (Gradstein - Ogg 1996), the age corresponds to the Lower Silurian Our data need a verification by another isotopic method because no Silurian magmatic activity within the Brunovistulicum has been supposed yet
    Česká geologická služba
Contributor code
    ČGS (UNM)
Source format
Entered date
    22. 1. 2008
Import date
    8. 8. 2012