Dyke to sill deflection in the shallow heterogeneous crust during glacier retreat: part II

Changes from dyke to sill propagation in the shallow crust are often caused by dissimilar layer properties. However, most previous studies have not considered the influence of glacial loading and unloading on dyke and sill deflection processes. Here, we attempt to collectively explore mechanical (la...

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Bibliographic Details
Published in:Bulletin of Volcanology
Main Authors: Drymoni, K, Tibaldi, A, Bonali, FL, Mariotto, FP
Other Authors: Bonali, F, Mariotto, F
Format: Article in Journal/Newspaper
Language:English
Published: Springer 2024
Subjects:
Online Access:https://hdl.handle.net/10281/474039
https://doi.org/10.1007/s00445-024-01732-w