Time-variable strain and stress rates induced by Holocene glacial isostatic adjustment in continental interiors

•Large-scale non-tectonic processes, (e.g., ice loading) may induce time-variable deformation across wide areas, beyond the directly loaded region.•While integrated strain (and stress) may remain low, instantaneous rates can be larger than background tectonic rates.•Non-tectonic modulation of the se...

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Veröffentlicht in:	Tectonophysics 2023-05, Vol.854, p.229815, Article 229815
Hauptverfasser:	Craig, T.J., Calais, E., Fleitout, L., Bollinger, L., Scotti, O.
Format:	Artikel
Sprache:	eng
Schlagworte:	Continental seismicity Environmental Sciences Intraplate deformation Postglacial deformation Strain-rates
Online-Zugang:	Volltext
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