We are improving our search experience. To check which content you have full access to, or for advanced search, go back to the old search.

Search

Please fill in this field.
Filters applied:

Search Results

Showing 1-13 of 13 results
  1. Recent Reactivation of Variscan Tectonic Zones: A Case of Rodl-Kaplice-Blanice Fault System (Bohemian Massif, Austria/Czech Republic)

    The Rodl-Kaplice-Blanice fault system (RKB) of Variscan shear origin, repeatedly active since the Late Paleozoic to the Recent, is expressed by a...

    Pavel Roštínský, Lubomil Pospíšil, ... Eva Nováková in Surveys in Geophysics
    Article Open access 22 February 2024
  2. New geophysical and geological data on the Moldanubian plutonic complex and the Kaplice Fault, southern Bohemia

    The paper presents a new structural model of the granitoid intrusions of the Moldanubian plutonic complex in southern Bohemiaeast of the town of...

    Melnyk Anastasiia, Černý Jan, ... Adamovič Jiří in International Journal of Earth Sciences
    Article 26 March 2022
  3. Geochronology and geochemistry of a dyke–host rock association and implications for the formation of the Bavarian Pfahl shear zone, Bohemian Massif

    To place constraints on the formation and deformation history of the major Variscan shear zone in the Bavarian Forest, Bavarian Pfahl zone, SW...

    Wolfgang Siebel, Ulrich Blaha, ... Johann Rohrmüller in International Journal of Earth Sciences
    Article 19 November 2004
  4. 40Ar/39Ar hornblende dating of a microgranodiorite dyke: implications for early Permian extension in the Moldanubian Zone of the Bohemian Massif

    Laser fusion 40 Ar/ 39 Ar ages of titanian pargasite from a microgranodiorite dyke swarm in the southern Bohemian Massif effectively date the early...

    J. Košler, S. Kelley, S. Vrána in International Journal of Earth Sciences
    Article 01 March 2001
  5. Stratigraphy

    The Moldanubian Zone of the Bohemian Massif represents a major crystalline segment within the eastern part of the mid-Paleozoic Variscan fold-belt....
    J. Fiala, G. Fuchs, J. I. Wendt in Pre-Permian Geology of Central and Eastern Europe
    Chapter 1995
  6. Structure

    The Moldanubian Zone (MZ) was considered for many decades as an old nucleus (median mass) of the Bohemian Massif consolidated during the Cadomian or...
    Chapter 1995
  7. Seismogeological acceptance criteria for geological repositories for spent nuclear fuel

    Qualitative geological acceptance criteria and quantitative seismological acceptance criteria for radioactive waste disposals are developed. The...

    Vladimír Schenk, Zdeňka Schenková, Pavel Kottnauer in Natural Hazards
    Article 01 September 1994
  8. Tectonometamorphic evolution of the Bohemian Massif: evidence from high pressure metamorphic rocks

    The Variscan orogenic belt, of which the Bohemian Massif is a part, is typically recognized for its characteristic low pressure, high temperature...

    P. J. O'Brien, D. A. Carswell in Geologische Rundschau
    Article 01 September 1993
  9. Variszische duktile Tektonik im Böhmischen Massiv

    The strain analysis and synthesis of the orientation distribution of stretching lineations and of foliations in the ductile domains of the Bohemian...

    Petr Rajlich in Geologische Rundschau
    Article 01 October 1987
  10. Hercynian-thrust related shear zones and deformation of the Varied Group on the contact of granulites/Southern Moldanubian, Bohemian Massif/

    The three deformation phases inferred from the detailed structural analysis of the Cesky Krumlov Varied Group record the Hercynian development of the...

    Petr Rajlich, Jaroslav Synek, ... Karel Schulmann in Geologische Rundschau
    Article 01 October 1986
  11. Seismic hazard estimate for a low seismicity region — Example of Bohemia

    The contribution reviews basic concepts of earthquake hazard assessment for sites of nuclear power plants. Taking into account the delineation of...

    Zdeňka Schenková, Vladimír Schenk, Vít Kárník in pure and applied geophysics
    Article 01 September 1981
  12. The Precambrian tectogenesis in the Bohemian Massif

    The Cadomian and Variscan tectogeneses are two distinctive and easily distinguished cycles of a long-term geological process leading to the almost...

    J. Chaloupský in Geologische Rundschau
    Article 01 February 1978
Did you find what you were looking for? Share feedback.