Fault populations, strain distribution and basement fault reactivation in the East Pennines Coalfield, UK
The scaling properties of faults within the East Pennine Coalfield (UK) are analysed for a fault population defined from a high quality, regional (ca. 1300 km 2) fault map for an Upper Carboniferous (Westphalian) coal seam. The fault system is dominated by an orthogonal network of NW- and NE-strikin...
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Veröffentlicht in: | Journal of structural geology 2005-05, Vol.27 (5), p.913-928 |
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Hauptverfasser: | , , |
Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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Zusammenfassung: | The scaling properties of faults within the East Pennine Coalfield (UK) are analysed for a fault population defined from a high quality, regional (ca. 1300
km
2) fault map for an Upper Carboniferous (Westphalian) coal seam. The fault system is dominated by an orthogonal network of NW- and NE-striking faults that preserve predominantly dip-slip extensional displacements ranging from |
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ISSN: | 0191-8141 1873-1201 |
DOI: | 10.1016/j.jsg.2004.10.014 |