Podrobnosti záznamu

Název
    GeoErlangen 2005, System Earth-Biosphere Coupling, Regional geology of Central Europe, September 24-29, 2005, Erlangen, Germany : International Conference and Annual Meeting Geologische Vereinigung (GV), Deutsche Gesellschaft für Geowissenschaften (DGG) at the Friedrich-Alexander-University Erlangen-Nuremberg, Germany : Exkursionsführer - Excursion guide (Variant.)
Další názvy
    The KTB deep crustal laboratory and the western Eger Graben
    The KTB deep crustal laboratory and the western Eger Graben. Geology and active geodynamics of the western Eger Rift area
    The KTB deep crustal laboratory and the western Eger Graben. Second day: Active processes of the western Eger Graben area : introduction
    The KTB deep crustal laboratory and the western Eger Graben. Second day: Active processes of the western Eger Graben area : stop 6a-c
    The KTB deep crustal laboratory and the western Eger Graben. Second day: Active processes of the western Eger Graben area : stop 7a, b
    The KTB deep crustal laboratory and the western Eger Graben. Second day: Active processes of the western Eger Graben area. stop 8
    The KTB deep crustal laboratory and the western Eger Graben. Second day: Active processes of the western Eger Graben area. Stop 9
    The KTB deep crustal laboratory and the western Eger Graben. Third day: (A) Geodynamic observation of fluid driven earthquake swarms and mantle fluid transport processes in the Nový Kostel epicentral area : introduction
    The KTB deep crustal laboratory and the western Eger Graben. Third day: (A) Geodynamic observation of fluid driven earthquake swarms and mantle fluid transport processes in the Nový Kostel epicentral area : stop 10
    The KTB deep crustal laboratory and the western Eger Graben. Third day: (A) Geodynamic observation of fluid driven earthquake swarms and mantle fluid transport processes in the Nový Kostel epicentral area : stop 12
    The KTB deep crustal laboratory and the western Eger Graben. Third day: (A) Geodynamic observation of fluid driven earthquake swarms and mantle fluid transport processes in the Nový Kostel epicentral area. Stop 11