Refining the Extent and Depth of the Shear Zone Surrounding the Alpine Fault Using Receiver Function Harmonics

Abstract Large continental transform faults are thought to cross‐cut the crust and extend into the lithospheric mantle. However, the strain distribution associated with these faults at mantle depths is not well understood. At the heart of this question is the rheology of the lithosphere: when stress...

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Bibliographic Details
Main Author: Hannah F. Mark
Format: Article
Language:English
Published: Wiley 2024-12-01
Series:Geophysical Research Letters
Online Access:https://doi.org/10.1029/2024GL112092
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