Podrobnosti záznamu

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    Cyclic evolution of convergent plate margins indicated by time sequence of volcanism and subduction
    Cyclic evolution of convergent plate margins indicated by time sequence of volcanism and subduction
    How did the calcareous nannoplankton assemblages reflect the paleoenvironmental changes indicated by mass mortality of Early Oligocene pteropods
    Magma Flow Direction in Dikes as Indicated by Magnetic Anisotropy: Examples from Dike Swarms of Bohemian Massif and Namibian Margin
    Magnetic fabric and weak deformation in sandstones of accretionary prism of the Flysch and Klippen Belts of the Western Carpathians: Mostly offscraping indicated
    Magnetic fabric and weak deformation in sandstones of accretionary prisms of the Flysch and Klippen Belts of the Western Carpathians: Mostly offscraping indicated
    Neogene Deformations of the Core Mountains of the Central Western Carpathians as Indicated by Magnetic Anisotropy
    Recent Tectonic Movements in the NE Part of the Bohemian Massif, Czech Republic, Indicated by the Brittle Tectonic Approach
    Tectonic interaction between the internides and centralides of the Inner West Carpathians, as indicated by magnetic anisotropy