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Fault and folding

Earth 238-23. Fault and folding. *Fault-bend folds. Earth 238-23. Fault and folding. Earth 238-23. Fault and folding. Earth 238-23. Fault and folding. Earth 238-23. Fault and folding. *Fault-bend folds develop in normal fault systems, most notably rollover anticlines. Earth 238-23.

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Fault and folding

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  1. Earth 238-23 Fault and folding *Fault-bend folds

  2. Earth 238-23 Fault and folding

  3. Earth 238-23 Fault and folding

  4. Earth 238-23 Fault and folding

  5. Earth 238-23 Fault and folding *Fault-bend folds develop in normal fault systems, most notably rollover anticlines.

  6. Earth 238-23 Faulting and stress

  7. Earth 238-23 Faulting and stress

  8. Earth 238-23 Faulting and stress

  9. Earth 238-23 Fault systems

  10. Earth 238-23 Fault systems: normal fault

  11. Earth 238-23 Fault systems: normal fault

  12. Earth 238-23 Fault systems: reverse fault *Duplex system : Fold and thrust belt, thin-skinned tectonic.

  13. Earth 238-23 Fault systems: reverse fault

  14. Earth 238-23 Fault systems: reverse fault « In sequence » thrusts: The thrusts tend to break forward towards the basin because it is composed of sediment weaker than that incorporated in the thrust system. « Out-of-sequence » thrusts: thrusts that form later in the interior of the wedge of previously thrust-faulted material.

  15. Earth 238-23 Fault systems: reverse fault

  16. Earth 238-23 Fault systems: strike-slip fault *Restraining or compressional bends- folds and thrusts. *Releasing or extensional bends- normal faults and grabens

  17. Earth 238-23 Fault systems: strike-slip fault

  18. Earth 238-23 Fault systems: strike-slip fault

  19. Earth 238-23 Fault systems: strike-slip fault *Flower structure

  20. Earth 238-23 Transpression-Transtension *Transpression *Transtension Transpression or compression normal to the fault during strike-slip. Transtension or extension normal to the fault during strike-slip. Can be used to describe motion across entire strike-slip fault zone, or that with in bends. Produces similar structures to restraining or releasing bends in strike-slip faults.

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