Impact of far-field glacially-induced stresses on fault stability in the eastern Paris Basin
Stable Continental Regions (SCR) feature very low seismicity levels, but historical seismicity reveals that these areas can experience large damaging earthquakes of magnitude up to Mw ≈ 7, on faults that were previously undocumented or thought to be stable. Glacial Isostatic Adjustment (GIA) is comm...
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Veröffentlicht in: | Tectonophysics 2023-10, Vol.864, p.230035, Article 230035 |
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