Record details

Title
    Lithofacies and Cyclic Development of Turbidite Systems in the Mírov Culm and the Southern Part of Zábřeh Crystalline Complex
Statement of responsibility
    Martin Janoška, Ondřej Bábek
Author
    Bábek, Ondřej, 1969-
    Janoška, Martin
Language
    anglicky
Source title - serial
    Věstník Českého geologického ústavu (Bulletin of the Czech Geological Survey)
Vol./nr.
    Vol. 73, no. 1
Pages
    p. 15-22
Year
    1998
Notes
    5 obr., 1 fot., 1 pl., 39 bibl.
    České resumé
    Zkr. název ser.: Věst. Čes. geol. Úst. (Bull. Czech geol. Surv.)
Subject group
    cyklus sedimentační
    flyš
    karbon-spodní
    moravskoslezské prevariské paleozoikum
    sedimentace hlubokomořská
    sedimentace siliciklastická
    sedimenty klastické
    turbidit
    zábřežské krystalinikum
Geographical name
    ČR-Morava
    Mírov (Šumperk)
    Zábřeh (Šumperk)
Keyword
    Complex
    Crystalline
    Culm
    Cyclic
    Development
    Lithofacies
    Mírov
    Southern
    Systems
    Turbidite
    Zábřeh
Abstract (in english)
   The Mírov Culm and the southern part of the Zábřeh Crystalline Complex near Hoštejn are composed of a succession of siliciclastic turbidites that show a striking similarity both in lithofacies composition and meso- to microscale cyclic development. Facies characteristics, trace fossil assemblages and the occurrence of distinct, fining- and thinning-upward autocyclic units point to the deposition at intermediate depths in submarine middle fan environment. Previously published sparse biostratigraphic data and the similar depositional setting may indicate both the areas to represent tectonic relics of the earliest, westernmost deep-marine depocentre of the Moravo-Silesian Culm siliciclastic system
Contributor
    Česká geologická služba
Contributor code
    ČGS (UNM)
Source format
    U
Entered date
    31. 3. 2008
Import date
    8. 8. 2012