Faults of the Bohemian Massif
Source of Analytical Data on Main Faults and Faulted Areas with Seismic Potential
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dbz:diendorf-boskovice_fault
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dbz:diendorf-boskovice_fault [2021/04/29 15:45] petrs [Quaternary] |
dbz:diendorf-boskovice_fault [2021/04/29 15:46] petrs [Quaternary] |
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| *In the southern part of DBF, the sections DF_1 to BF_2 are ranked **class 3**, i.e. assumed or admitted to be active but without direct evidence. Quaternary slip rate at fault sections north of DF_3 is assumed very low (<0.01 mm/y). Southern sections may later be ranked class 1 (demonstrably active) when new earthquake data (better location, focal mechanism) bring clear evidence. | *In the southern part of DBF, the sections DF_1 to BF_2 are ranked **class 3**, i.e. assumed or admitted to be active but without direct evidence. Quaternary slip rate at fault sections north of DF_3 is assumed very low (<0.01 mm/y). Southern sections may later be ranked class 1 (demonstrably active) when new earthquake data (better location, focal mechanism) bring clear evidence. | ||
| *In the northern part of DBF, the sections BF_3 to BF_ 17 are ranked **class 4**, i.e. assumed or demonstrated to be inactive. | *In the northern part of DBF, the sections BF_3 to BF_ 17 are ranked **class 4**, i.e. assumed or demonstrated to be inactive. | ||
| - | On a theoretical basis, the evaluation of similarly oriented | + | On a theoretical basis, the evaluation of similarly oriented sections |
| -expected northward decrease of rate of stress build-up (and hence crustal strain rate), and | -expected northward decrease of rate of stress build-up (and hence crustal strain rate), and | ||
| -expected northward decrease of slip potential due to rotation of stress orientation near junction of the Alpine and the West-European stress domains. | -expected northward decrease of slip potential due to rotation of stress orientation near junction of the Alpine and the West-European stress domains. | ||
dbz/diendorf-boskovice_fault.txt ยท Last modified: 2024/05/29 16:39 by petrs
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