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  2. File:Fault Map-1.pdf - Wikipedia

    en.wikipedia.org/wiki/File:Fault_Map-1.pdf

    Short title: Fault Map#1; Unique ID of original document: xmp.did:b77bd4f0-4937-9d4d-b8cf-746d273c01d8: Software used: Adobe Illustrator CC 2014 (Windows)

  3. Bow-tie diagram - Wikipedia

    en.wikipedia.org/wiki/Bow-tie_diagram

    A bow-tie diagram is a graphic tool used to describe a possible damage process in terms of the mechanisms that may initiate an event in which energy is released, creating possible outcomes, which themselves produce adverse consequences such as injury and damage. The diagram is centred on the (generally unintended) event with credible initiating ...

  4. Fault (geology) - Wikipedia

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

    A fault plane is the plane that represents the fracture surface of a fault. A fault trace or fault line is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. [3] [4] A fault zone is a cluster of parallel faults.

  5. File:T-S diagram.pdf - Wikipedia

    en.wikipedia.org/wiki/File:T-S_diagram.pdf

    Original file (1,443 × 816 pixels, file size: 66 KB, MIME type: application/pdf) This is a file from the Wikimedia Commons . Information from its description page there is shown below.

  6. Sinistral and dextral - Wikipedia

    en.wikipedia.org/wiki/Sinistral_and_dextral

    Schematic illustration of the two strike-slip fault types. The view is of the Earth's surface from above. In geology, the terms sinistral and dextral refer to the horizontal component of the movement of blocks on either side of a fault or the sense of movement within a shear zone. These are terms of relative direction, as the movement of the ...

  7. Fold (geology) - Wikipedia

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

    Fault-bend folds are caused by displacement along a non-planar fault. In non-vertical faults, the hanging-wall deforms to accommodate the mismatch across the fault as displacement progresses. Fault bend folds occur in both extensional and thrust faulting. In extension, listric faults form rollover anticlines in their hanging walls. [11]

  8. Anderson's theory of faulting - Wikipedia

    en.wikipedia.org/wiki/Anderson's_Theory_of_Faulting

    Anderson's fault theory also presents a model for seismic interpretation. [7] This model predicts the dip of faults according to their regime classification. [2] Conjugate walls in any fault will share a dip angle with that angle being measured from the top of the hanging wall or the bottom of the foot wall. [2]

  9. File:Original McKelvey Diagram 1976.pdf - Wikipedia

    en.wikipedia.org/wiki/File:Original_McKelvey...

    Original_McKelvey_Diagram_1976.pdf (725 × 591 pixels, file size: 147 KB, MIME type: application/pdf) This is a file from the Wikimedia Commons . Information from its description page there is shown below.