Published online by Cambridge University Press: 02 December 2021
The most prominent fault scarps are found in northern Fennoscandia in the northernmost parts of Norway, Sweden and Finland. In addition, signs of glacially triggered faulting were identified in adjacent Russia. The following chapters give an overview about these faults from their identification until the very recent results that include, among other things, new reactivation dating and revised fault geometries at the surface from laser scanning.
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