Record details

    Problematika regionální příslušnosti krystalinika České brány k saxothuringiku (02-43 Litoměřice)
Statement of responsibility
    Bedřich Mlčoch
Other titles
    Correlation of the crystalline basement outcropping in the Porta Bohemica with the Saxothuringian Unit
    Mlčoch, Bedřich
Source title - serial
    Zprávy o geologických výzkumech v roce 2002
    s. 31-32
    1 obr., 4 bibl.
    Anglické resumé
    Zkr. název ser.: Zpr. geol. Výzk. v Roce 2002.
Subject group
    geologie regionální
    kontrola tektonická
    mapa geologická
    tepelské krystalinikum
Geographical name
Abstract (in english)
   New information was obtained on the character of the contact between Saxothuringian (SU) and Teplá-Barrandian Units (TBU) in the area between Karlovy Vary and Litoměřice in relation to construction of elevation model of the crystalline basement (MLČOCH ed. 2001) and new geological mapping at a scale of l : 10 000 of crystalline outcrops in Porta Bohemica. The succession granulite-orthogneiss-mica schist/paragneiss-phyllite/metabasite was established on the southeastern border of SU on several localities between Doupov and Litoměřice. Some phyllite outcrops, known before, were usually considered as Lower Palaeozoic in age, belonging to SU. One of them was described by SATTRAN and VÁNĚ (1964) from Ohře Valley, actually at the bottom of the Nechranice Dam. A similar succession occurs also in Porta Bohemica near Litoměřice, and it is more probable that phyllites and amphibolites outcropping there belong to SU and not to TBU, as was considered by POUBOVÁ (1962)
    Česká geologická služba
Contributor code
    ČGS (UNM)
Source format
Entered date
    29. 5. 2007
Import date
    8. 8. 2012