Controls on spatial and temporal patterns of slope deformation in an Alpine valley
Résumé
• Seasonal pore pressure variations in fractured crystalline hillslope induce correlated reversible surface deformations • Decameter-scale brittle-ductile faults control local spatial variations of deformation patterns • Cyclic groundwater pressure-related rock mass fatigue induces irreversible gravitationallydriven displacements in valley slopes *
Domaines
Sciences de la Terre
Fichier principal
JGR Earth Surface - 2021 - Oestreicher - Controls on Spatial and Temporal Patterns of Slope Deformation in an Alpine Valley.pdf (8.6 Mo)
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