A significant period of increased tectonics was monitored between 2013 and 2015 on the eastern margin of the Bohemian Massif along ten faults. Nine of them showed a uniform scheme: dextral strike-slip along generally NW–SE striking faults, sinistral strike-slip along generally NE-SW striking faults and uprising of the southern blocks. The distinguished fault displacements displayed an NNW-SSE striking compressional component of the stress field during this remarkable tectonic episode.
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