Source of Analytical Data on Main Faults and Faulted Areas with Seismic Potential
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dbz:diendorf-boskovice_fault [2020/05/29 16:02] petrs |
dbz:diendorf-boskovice_fault [2021/04/29 15:45] petrs [Quaternary] |
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* Results of some long-term geodetic measurements in the region were interpreted as tectonic deformation in several studies (Pospíšil et al. 2009, 2010, 2012; Roštínský et al. 2013). However, editor of this text is skeptical to interpretation of these observations as due to tectonic strain because: | * Results of some long-term geodetic measurements in the region were interpreted as tectonic deformation in several studies (Pospíšil et al. 2009, 2010, 2012; Roštínský et al. 2013). However, editor of this text is skeptical to interpretation of these observations as due to tectonic strain because: | ||
- | - the reported strain rates are too large (10< | + | - the reported strain |
- the locally observed geological records rule out that such deformation at BF could have been operative on a long-term scale during Quaternary; | - the locally observed geological records rule out that such deformation at BF could have been operative on a long-term scale during Quaternary; | ||
- | - the non-tectonic deformation (climatic/ | + | - the non-tectonic deformation (climatic/ |
:!: **Basing on this local evidence the fault activity is currently evaluated in a following way:** | :!: **Basing on this local evidence the fault activity is currently evaluated in a following way:** |