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  2. Anderson's theory of faulting - Wikipedia

    en.wikipedia.org/wiki/Anderson's_Theory_of_Faulting

    Dip is defined as the angle of the fault relative to the surface of the earth, which indicates the plane on which slip will occur. Lastly, in any non-vertical fault, the block above the fault is called the hanging wall, while the blockbelow the fault is called the footwall. [4] Normal and reverse dip-slip faults with labeled hanging wall and ...

  3. Fault (geology) - Wikipedia

    en.wikipedia.org/wiki/Fault_(geology)

    The hanging wall occurs above the fault plane and the footwall occurs below it. [14] This terminology comes from mining: when working a tabular ore body, the miner stood with the footwall under his feet and with the hanging wall above him. [15] These terms are important for distinguishing different dip-slip fault types: reverse faults and ...

  4. Focal mechanism - Wikipedia

    en.wikipedia.org/wiki/Focal_mechanism

    In the case of a fault-related event, it refers to the orientation of the fault plane that slipped, and the slip vector and is also known as a fault-plane solution. Focal mechanisms are derived from a solution of the moment tensor for the earthquake, which itself is estimated by an analysis of observed seismic waveforms. The focal mechanism can ...

  5. Control reconfiguration - Wikipedia

    en.wikipedia.org/wiki/Control_reconfiguration

    Control reconfiguration is an active approach in control theory to achieve fault-tolerant control for dynamic systems. [1] It is used when severe faults , such as actuator or sensor outages, cause a break-up of the control loop , which must be restructured to prevent failure at the system level.

  6. Transpression - Wikipedia

    en.wikipedia.org/wiki/Transpression

    A fault bend, or fault stepover, forms when individual segments of the fault overlap and link together. The type of structures which form along the strike-slip fault depend on the sense of slip relative to the sense of stepping. When a sinistral fault steps to the right or a dextral fault steps to the left, a restraining bend is formed. [2]

  7. Inversion (geology) - Wikipedia

    en.wikipedia.org/wiki/Inversion_(geology)

    The likelihood of fault reactivation depends on the dip of the existing fault plane. Lower angle faults are more favourable as the resolved shear stress on the plane is higher. When a listric fault , which increases in dip upwards, reactivates the uppermost part of the fault may be too steep and new reverse faults typically develop in the ...

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  9. Fault model - Wikipedia

    en.wikipedia.org/wiki/Fault_model

    A fault model, falls under one of the following assumptions: single fault assumption: only one fault occur in a circuit. if we define k possible fault types in our fault model the circuit has n signal lines, by single fault assumption, the total number of single faults is k×n. multiple fault assumption: multiple faults may occur in a circuit.