Record details

    Petrogenetic relationship between deformation and alteration on the example of the extension tectonics of the Veporicum crystalline basement (Central Western Carpathians)
Statement of responsibility
    Pavol Siman, Ján Madarás, Martin Kováčik, Karel Schulmann, Patrick Ledru
    Kováčik, Martin
    Ledru, Patrick
    Madarás, Ján
    Schulmann, Karel
    Siman, Pavol
Source title - serial
    Slovak geological magazine
    No. 3-4
    p. 175-178
    2 obr., 21 bibl.
    Zkr. název ser.: Slov. geol. Mag.
Subject group
    minerály horninotvorné
    podmínky P-T
    vrásnění alpinské
    vrásnění variské
Geographical name
Abstract (in english)
   The conditions of the deformation in the Veporicum crystalline basement are estimated at middle to upper greenschist facies or the lower part of amphibolite facies; according to these first results, max. T reached approximatelly -450-500 C at P- 3-4 kbar. The observations from the Permo-Mesozoic cover sediments suggest that deformation occurred in the greenschist facies conditions at a temperature estimated at 350 C (max. 450 C according to crystal plasticity of quartz in the eastern part), or only at anchimetamorphism. Our observations suggest that the major paragenetic transformations reflect probably the strong Alpine overprint. We assume that only relics of higher metamorphosed rocks from the so-called "hybridic complex" in the southern part of the Veporicum basement could bear records of Late-Hercynian events
    Česká geologická služba
Contributor code
    ČGS (UNM)
Source format
Entered date
    21. 3. 2008
Import date
    8. 8. 2012