The Role of Sinistral Strike-Slip Faults in the Formation of the Structural Fabric of the Slavonian Mts. (Eastern Croatia)

摘要: This paper presents a simplified evolution for the Slavonian Mts. structural fabric during Neogene, emphasising importance of sinistral wrench faults. These faults were formed under influence dextral displacements along stretching through Drava and Sava. They caused uplift compression general area events accompanied by folding, reverse faulting counter-clockwise rotation uplifted structures, typical transpression model tectonic processes.