Tilted Fault Blocks are referred to as rotational block faulting or blocks. They are created during extensional tectonic processes where the crust tilts and the brittle crust splits as a result of extension, causing detachment faults.
Tilted block faulting, often referred to as rotational block faulting, is a process of structural evolution that occurs as tectonic plates split during extensional tectonic events. When extensional pressures are applied to the upper lithospheric crust, detachment faults are created. The ductile bottom crust ascends as a result of these typical faults, and the higher crust fractures into tilted fault blocks. The outcome is the lifting, cooling, and exhumation of ductile deformed deeper crust. The significant group of slanted blocks and associated crust may constitute a sizeable percentage of the metamorphic core complexes, which are found in both the continental and oceanic crust.
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