Notes and questions
Development of the Structure and Granite Emplacement along the Boundary between Vepor and Gemer Units (Western Carpathians)
Graphite as a source of information concerning the genesis of some deposits in the Spiš Gemer Ore Mts.
New Approach to Interpretation of Superposed Cleavage Patterns in Weak Rocks result of Independent Movements of Rigid Basement Promotories on an Example of the Gemer Unit
Syntectonic Emplacement of Leucogranitic Magma during Oblique Transpression: the Boundary between the Vepor and Gemer Units (West Carpathians)