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A detachment fault is a gently dipping normal fault associated with large-scale extensional tectonics. Detachment faults often have very large displacements and juxtapose unmetamorphosed hanging walls against medium to high-grade metamorphic footwalls that are called metamorphic core complexes. They are thought to have formed as either initially low-angle structures or by the rotation of initially high-angle normal faults modified also by the isostatic effects of tectonic denudation. They may also be called denudation faults.
Examples of detachment faulting include:The Snake Range detachment system of the Basin and Range Province of western North America which was active during the Miocene
The Nordfjord-Sogn detachment of western Norway active during the Devonian Period
The Whipple detachment in southeastern California
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