Normal Fault Diagram

Normal Fault Diagram. Normal faulting occurs when two plates move away from each other, causing one to slide down relative to. A diagram outlining the basics of faulting.

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In a normal fault the hanging wall slips beneath the foot wall. Groups of normal faults can produce horst and graben topography, or a series of relatively high- and low-standing fault blocks, as seen in areas where the crust is rifting or being pulled apart by plate. Block diagram of single rectangular normal fault showing. slip direction and geometry parameters: fault length L Normal, or Dip-slip, faults are inclined fractures where the blocks have mostly shifted vertically.

Abstract Increased interest in normal faults and extended terranes has led to the development of an increasingly complex terminology.

Where the fault plane is sloping, as with normal and reverse faults, the upper side is the hanging wall and the lower side is the footwall.

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Block diagram of single rectangular normal fault showing. slip direction and geometry parameters: fault length L Normal, or Dip-slip, faults are inclined fractures where the blocks have mostly shifted vertically. A fault is a fracture, or break, in the Earth's crust (lithosphere). This chapter introduces basic fault tree analysis and points out the similarities (and differences) between RBDs and fault tree diagrams.

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