Podrobnosti záznamu

Název
    Translational Block-Type Slope Movements - Mechanism and Examples
Údaj o odpovědnosti
    Juliane Heiland
Další názvy
    Translační svahové pohyby blokového typu, jejich mechanismus a příklady
Autor
    Heiland, Juliane
Jazyk
    anglicky
Zdrojový dokument - seriál
    Acta montana. Series AB
Svazek/č.
    No. 6(109)
Strany
    p. 81-137
Rok
    1998
Poznámky
    15 obr., 3 tab., 6 s.bibl.
    České resumé
    Zkr. název ser.: Acta montana (Praha), Ser. AB
Předmětová skupina
    dizertace
    flyšové pásmo Západních Karpat
    geomorfologie
    kladensko-rakovnická pánev
    mapa inženýrskogeologická
    plasticita
    plocha smyková
    pohyb svahový
    rychlost
    sesuv
    srážky dešťové
    terminologie
Geografické jméno
    ČR
    Itálie severní
    Mladotice (Plzeň-sever)
    Potvorov (Plzeň-sever)
    Rakousko
    Šance (Frýdek-Místek)
Klíčové slovo
    Block-Type
    Examples
    Mechanism
    Movements
    Slope
    Translational
Abstrakt (anglicky)
   This publication summarized a doctoral thesis, which had been worked out between 1994-1997 within external postgradual studies at the Faculty of Sciences, Charles University and at the Department of Engineering Geology, Institute of Rock Structure and Mechanics, Czech Academic Exchange Service (DDAS) and by the European Commission, Supplementary, Agreement No ERBCIPDCT 930052 to contract No ERBEV5VCT 920180. The theme of this work is translational block-type slope movements and their mechanism, as could be examined in several field areas. My method of working was firstly extnesive field mapping of the geological and geomorphological conditions of the slope movement areas along profiles taken during field work and thus I tried to establish a possible explanation for the slope movement evolution and mechanism of each fields area.
   In the case of one field area in the Moravskoslezské Beskydy Mountains this did not lead to a satisfying result and I decided to do physical modeling on this particular area with the help of my colleague B. Košťák. In the last stage of my work I tried to establish general throughts about the definition, mechanism and characteristics of translational block-type slope movements. A result of this work is a new interpretation of the slope movement area Lukšinec Hill in the Moravskoslezské Beskydy Mountains, which is mainly based on a different geological build-up than was described by Novosad (1966, 1978, 1993) in previous works. In the slope movement area Potvorský kopec, situated in the Kladno-Rakovník Permocarboniferous fault-basin, several stages of slope movement activity could be distinguished, which culminated in an disastrous landslide in 1872.
   In Austria, I studied two fields areas siatuated in a similar geology with both showing translational block-type slope movement development in a pronounced form. A large part of this thesis is concerned with the comparison of Řečice lanslide in the Beskydy Mountains with similar slope movements in the Langhe-Cunesi region in Northern Italy. In t
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    25. 3. 2008
Datum importu
    8. 8. 2012