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Geology 360 - Introduction to Strike-Slip Faults

Geology 360 - Introduction to Strike-Slip Faults. Levant Strike-Slip Faults. Left-lateral strike-slip Levant fault, plate boundary between Arabia and Africa. San Andreas from Space. Two northwest-southeast-trending faults are visible.

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Geology 360 - Introduction to Strike-Slip Faults

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  1. Geology 360 - Introduction to Strike-Slip Faults

  2. Levant Strike-Slip Faults Left-lateral strike-slip Levant fault, plate boundary between Arabia and Africa

  3. San Andreas from Space • Two northwest-southeast-trending faults are visible. • The Hayward Fault, bordering the urban area east of San Francisco Bay • The San Andreas Fault, crossing the mid-San Francisco Peninsula before dipping beneath the Pacific Ocean and surfacing again northwest of Golden Gate Bridge San Francisco Bay, California.

  4. San Andreas fault, western North America

  5. Outline • Stick-Slip and Creep • Andersonian Theory • Kinematics • Strike-Slip Faults on Continental Margins • Strike-Slip Faults on Mid-Ocean Ridges

  6. Stick-Slip: Elastic Rebound Theory D

  7. Elastic Rebound Theory • Imagine a fence across an active fault

  8. Elastic Rebound Theory • Imagine a fence across an active fault • Regional deformation occurs but the fault does not break. The fence becomes curved.

  9. Elastic Rebound Theory • Imagine a fence across an active fault • Regional deformation occurs but the fault does not break (locked fault) • Once the fault breaks, the fence is sheared in half and marks offset • The far-field strain may limit whether the fault accommodates all the plate motion at its trace

  10. Elastic Rebound Theory

  11. Elastic Rebound Theory

  12. Creep (Aseismic Slip) • Imagine a fence across an active fault • Slip occurs slowly on the fault continually over time (fault is not locked) • Creeping faults do not store elastic energy that might be released by a stick-slip event (an earthquake)

  13. Andersonian Theory

  14. Conjugate Strike-Slip Faults

  15. Determining Sense of Slip

  16. Right-Lateral (Dextral)

  17. Left-Lateral (Sinistral)

  18. Arrow Heads ( ) and Tails ( ) Block moving toward you like an arrowhead heading towards you Block moving away from you like seeing the feathers of an arrow

  19. Arrow Heads ( ) and Tails ( ) Right-lateral or left-lateral?

  20. Arrow Heads ( ) and Tails ( ) Left-lateral

  21. Arrow Heads ( ) and Tails ( ) Sinistral or Dextral?

  22. Arrow Heads ( ) and Tails ( ) Dextral

  23. Strike-Slip Faulting: Shallow Brittle vs Deep Shear

  24. Strike-Slip Faulting: EQ’s = dislocations http://www.data.scec.org/Module/links/landrupt.html Landers rupture propagation movies

  25. Strike-Slip Faulting: EQ’s = dislocations

  26. Strike-Slip Faulting: EQ’s = dislocations

  27. Strike-Slip Faults on Continental Margins 50 m N What is the sense of slip?

  28. Strike-Slip Faults on Continental Margins 50 m N Right-lateral (dextral)

  29. Transtension

  30. Development of a Pull-Apart Basin

  31. Pull-Apart Basin

  32. Initial Releasing Bend

  33. Evolution of a Releasing Bend

  34. Normal (-) Flower Structure - Tulip

  35. Transpression

  36. Development of a Restraining Bend

  37. Development of a Restraining Bend

  38. Initial Restraining Bend

  39. Evolution of a Restraining Bend

  40. Reverse (+) Flower Structure - Palm

  41. Summary of Flower Structures - Palms & Tulips

  42. Summary of Step Overs - Strike-Slip Faults

  43. Los Angeles - Pull apart structure Releasing bend

  44. Summary of Flower Structures - Palms & Tulips

  45. Summary of Flower Structures - Palms & Tulips

  46. Summary of Flower Structures - Palms & Tulips

  47. Summary of Flower Structures - Palms & Tulips

  48. Oceanic Strike Slip fault: Transforms

  49. Strike-Slip Faults on Mid-Ocean Ridges What is the sense of slip?

  50. Strike-Slip Faults on Mid-Ocean Ridges Right-lateral (Dextral)

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