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Peak frequency as noted on a radiation curve is directly proportional to the
Normal Fault
A type of fault where the hanging wall slides downward relative to the footwall due to tensile stress in the Earth's crust.
Strike-Slip Fault
A type of fault in which two blocks of the Earth's crust slide past each other horizontally along the fault plane.
Reverse Fault
A type of fault where the hanging wall moves up relative to the footwall, often created by compressive forces.
Normal Fault
A type of fault where the hanging wall has moved downward relative to the footwall, typically associated with extensional tectonics.
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