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Suppe, 1983

Suppe, 1983. Suppe, 1983. Advantages: Can be reconstructed from surface geology Assumptions: Pervasive slip on bedding planes as rocks pass through hinges Slip is carried off-section. Suppe, 1983. Suppe, 1983. Brown, GSA Mem 171, 1988. Brown, GSA Mem 171, 1988.

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Suppe, 1983

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  1. Suppe, 1983

  2. Suppe, 1983

  3. Advantages: Can be reconstructed from surface geology Assumptions: Pervasive slip on bedding planes as rocks pass through hinges Slip is carried off-section Suppe, 1983

  4. Suppe, 1983

  5. Brown, GSA Mem 171, 1988

  6. Brown, GSA Mem 171, 1988

  7. Rattlesnake Mtn interpretation of Sterns, 1971 Brown, GSA Mem 171, 1988

  8. Rattlesnake Mtn interpretation of Brown, 1984 Rattlesnake Mtn interpretation of Sterns, 1971 Brown, GSA Mem 171, 1988

  9. Brown, GSA Mem 171, 1988 Rattlesnake Mtn interpretation of Brown, 1984 Rattlesnake Mtn interpretation of Sterns, 1971 Rattlesnake Mtn interpretation of Erslev, 1986 Erslev, Geology, 1986

  10. Erslev, 1991

  11. Erslev, 1991

  12. Erslev, 1991

  13. Advantages: Deals with more realistic geometries in foreland situations than fault-bend folds Disadvantages: Requires plastic deformation in trishear zone, which can become non-unique in terms of structures Erslev, 1991

  14. Smithson et al., JGR, 1979

  15. Smithson et al., Geology, 1978

  16. Smithson et al., Geology, 1978

  17. Erslev, Geology, 1986

  18. Brown, GSA Mem 171, 1988 • Other shortening estimates: 60-120 km by Chapin and Cather (1983) to NNE • 43-52 km to ENE (Bird, 1998)

  19. Erslev, GSA SP 280, 1993

  20. Erslev, & Koenig, GSA Mem 204, 2009

  21. Erslev, & Koenig, GSA Mem 204, 2009

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