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    Propagation of coastal slope deformations at Taukliman, Bulgaria

    New search for: Košťák, B.
    New search for: Avramova-Tačeva, Elka

    Summary In a coastal region of high seismicity a giant block-type slope deformation is being propagated in sliding cycles due to the action of creep in a bed of clay, deep under a brittle rock platform.

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    Propagation of coastal slope deformations at Taukliman, Bulgaria

    New search for: Košťák, B.
    New search for: Avramova-Tačeva, Elka

    Summary In a coastal region of high seismicity a giant block-type slope deformation is being propagated in sliding cycles due to the action of creep in a bed of clay, deep under a brittle rock platform.

    Access

    Access via TIB
    Check availability in my library
    Order at Subito €

    Propagation of coastal slope deformations at Taukliman, Bulgaria

    New search for: Košťák, B.
    New search for: Avramova-Tačeva, Elka

    Summary In a coastal region of high seismicity a giant block-type slope deformation is being propagated in sliding cycles due to the action of creep in a bed of clay, deep under a brittle rock platform.

    Access

    Access via TIB
    Check availability in my library
    Order at Subito €

    Access

    Access via TIB
    Check availability in my library
    Order at Subito €

    Page navigation

    Document information
    Similar titles

    Export, share and cite

    Document information
    Title:

    Propagation of coastal slope deformations at Taukliman, Bulgaria

    Contributors:

    Košťák, B. (author) / Avramova-Tačeva, Elka (author)

    Published in:

    Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur ; 23

    Publication date:

    1981

    ISSN:

    0074-1612

    DOI:

    https://doi.org/10.1007/BF02594728

    Type of media:

    Article (Journal)

    Type of material:

    Print

    Language:

    English

    Keywords:

    Fracture Initiation , Coastal Slope , Secondary Creep , Vrancea Earthquake , Slope Deformation

    Classification:

    BKL:  38.58 Geomechanik / 56.20 Ingenieurgeologie, Bodenmechanik
    Local classification TIB:  050/6545

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