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Cited by 85

The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.

Dynamic and kinematic growth and change of a Coulomb wedge

Willett, Sean D.·1992·Thrust Tectonics
DOI 10.1007/978-94-011-3066-0_2
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Crossref · 10.1007/978-94-011-3066-0_2

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1 of 1 references verified0 citation errors · 0 not checkable

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  • The formation of the lower thrust system could have been driven by a progressive increase in the strength of the base of the wedge due to incorporation of the Archean basement, and/or by the large difference in thickness of the Knob Lake Group stratigraphy in the southeast compared to the northwest.

    “This could have been driven by a progressive increase in the strength of the base of the wedge [Willett, 1992] due to incorporation of the Archean basement, and/or as a result of the large difference in thickness of the Knob Lake Group stratigraphy in the southeast (slope deposits !2 km thick) compared to the northwest (platform deposits 200 m thick)”

    From Grenville Front zone, Gagnon terrane, southwestern Labrador: Configuration of a midcrustal foreland fold‐thrust belt (2008) · cites this paper as Willett, 1992

  • Analogue and numerical models indicate accretionary and orogenic wedges are dynamic phenomena that continually change their shape as new material is added to them.

    “Analogue and numerical models of accretionary and orogenic wedges indicate they are dynamic phenomena that continually change their shape as new material is added to them”

    From Grenville Front zone, Gagnon terrane, southwestern Labrador: Configuration of a midcrustal foreland fold‐thrust belt (2008) · cites this paper as Willett, 1992

Citations

Cites

Flagged first, then by citations

Research works printed but not linked: 33

  1. Barr, T. D. & Dahlen, F. A. 1989. Steady-State Mountain Building 2. Thermal Structure and Heat Budget. Journal of Geophysical Research, 94, 3923–3947. · DOI
  2. Beaumont, C., Hamilton, J. & Fullsack, P. 1991. Erosional Control of Active Compressional Orogens, this volume.
  3. Bird, P. & Piper, K. 1980. Plane Stress Finite Element Models of Tectonic Flow in Southern California. Physics of the Earth and Planetary Interiors, 21, 158–195. · DOI
  4. Borja, R. I. & Dreiss, S. J. 1989. Numerical Modelling of Accretionary Wedge Mechanics: Application to the Barbados Subduction Problem. Journal of Geophysical Research, 94, 9323–9339. · DOI
  5. Brandon, M. T. 1984. A study of deformational processes affecting unlithified sediments at active margins: A field study and a structural model, Ph.D. thesis, University of Washington, Seattle, 160p.
  6. Chapple, W. M. 1978. Mechanics of thin-skinned fold-and-thrust belts. Geological Society of America Bulletin, 89, 1189–1198. · DOI
  7. Cloos, M. 1982. Flow melanges: Numerical modelling and geologic constraints on their origin in the Franciscan subduction complex, California. Geological Society of America Bulletin, 93, 330–345. · DOI
  8. Cloos, M. 1984. Flow melanges and the structural evolution of accretionary wedges. Geological Society of America Special Paper, 198, 71–79. · DOI
  9. Cloos, M. & Shreve, R. L. 1988a. Subduction-Channel Model of Accretion, Melange Formation, Sediment Subduction, and Subduction Erosion at Convergent Plate Margins: 1. Background and Description. Pure and Applied Geophysics, 128, 455–500. · DOI
  10. Cloos, M. & Shreve, R. L. 1988b. Subduction-Channel Model of Accretion, Melange Formation, Sediment Subduction, and Subduction Erosion at Convergent Plate Margins: 2. Implications and Discussion. Pure and Applied Geophysics, 128, 501–545. · DOI
  11. Cowan, D. S. & Silling, R. M. 1978. A Dynamic, Scaled Model of Accretion at Trenches and Its Implications for the Tectonic Evolution of Subduction Complexes. Journal of Geophysical Research, 83, 5389–5396. · DOI
  12. Dahlen, F. A. 1984. Noncohesive Critical Coulomb Wedges: An Exact Solution. Journal of Geophysical Research, 89, 10125–10133. · DOI
  13. Dahlen, F. A., Suppe, J. & Davis, D. 1984. Mechanics of Fold-and Thrust Belts and Accretionary Wedges: Cohesive Coulomb Theory. Journal of Geophysical Research, 89, 10087–10101. · DOI
  14. Dahlen, F. A. & Barr, T. D. 1989. Steady-State Mountain Building 1. Deformation and Mechanical Energy Balance. Journal of Geophysical Research, 3906–3922.
  15. Davis, D., Suppe, J. & Dahlen, F. A. 1983. Mechanics of Fold-and-Thrust Belts and Accretionary Wedges. Journal of Geophysical Research, 88, 1153–1172. · DOI · Paper page
  16. Emerman, S. H. & Turcotte, D. L. 1983. A fluid model for the shape of accretionary wedges. Earth and Planetary Science Letters, 63, 379–384. · DOI
  17. Malvern, L.E. 1969. Introduction to the Mechanics of a Continuous Medium. Prentice-Hall, New Jersey.
  18. Moore, J. C., Watkins, J. S., Shipley, T. H., McMillen, K. J., Bachman, S. B., & Lundberg, N. 1982. Geology and tectonic evolution of a juvenile accretionary terrane along a truncated convergent margin: Synthesis of results from Leg 66 of the Deep Sea Drilling Project, southern Mexico. Geological Society of America Bulletin, 93, 847–861. · DOI
  19. Morley, C. K. 1988. Out-Of-Sequence Thrusts. Tectonics, 7, 539–561. · DOI
  20. Platt, J. P., Leggett, J. K., Young, J., Raza, H. & Alam, S. 1985. Large-scale sediment underplating in the Makran accretionary prism, southwest Pakistan. Geology, 13, 507–511. · DOI
  21. Platt, J. P. 1986. Dynamics of orogenic wedges and the uplift of high-pressure metamorphic rocks. Geological Society of America Bulletin, 97, 1037–1053. · DOI
  22. Platt, J. P. 1987. The uplift of high-pressure-low-temperature metamorphic rocks. Philosophical Transactions of the Royal Society of London A, 321, 87–103. · DOI
  23. Shi, Y. & Wang, C. 1988, Thermal Structure of the Barbados Accretionary Complex. Pure and Applied Geophysics, 128, 749–766. · DOI
  24. Silver, E. A., Ellis, M. J., Breen, N. A. & Shipley, T. H., 1985. Comments on the growth of accretionary wedges. Geology, 13, 6–9. · DOI
  25. Stockmal, G. S. 1983. Modelling of Large Scale Accretionary Wedge Deformation. Journal of Geophysical Research, 88, 8271–8287. · DOI
  26. Taylor, C. & Hughes, T. G. 1981. Finite Element Programming of the Navier-Stokes Equations. Pineridge Press Ltd., Swansea, UK, 244p.
  27. Vilotte, J. P., Daignieres, M. & Madariaga, R. 1982. Numerical Modelling of Interplate Deformation: Simple Mechanical Models of Continental Collision. Journal of Geophysical Research, 87, 10709–10728. · DOI
  28. Vilotte, J. P., Daignieres, M., Madariaga, R. & Zienkiewicz, O. 1984. The role of a heterogeneous inclusion during continental collision. Physics of the Earth and Planetary Interiors, 36, 236–259. · DOI
  29. Vilotte, J. P., Daignieres, M., Madariaga, R. & Zienkiewicz, O. 1986. Numerical study of continental collision: influence of buoyancy forces and an initial stiff inclusion. Geophysical Journal of the Royal Astronomical Society, 84, 279–310. · DOI
  30. Westbrook, G. K., Ladd, J. W., Buhl, P., Bangs, N. & Tiley, G. J. 1988. Cross section of an accretionary wedge: Barbados Ridge complex, Geology, 16, 631–635. · DOI · Paper page
  31. Zhao, W.-L., Davis, D. M., Dahlen, F. A. & Suppe, J. 1986. Origin of Convex Accretionary Wedges: Evidence From Barbados. Journal of Geophysical Research, 91, 10246–10258. · DOI
  32. Zienkiewicz, O.C. & Godbole, P. N. 1974. Flow of Plastic and Visco-Plastic Solids with Special Reference to Extrusion and Forming Processes. International Journal for Numerical Methods in Engineering, 8, 3–16.
  33. Zienkiewicz, O.C. 1977. The Finite Element Method. McGraw-Hill, New York, 851p.

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Metadata

Authors
Willett, S. D.
Venue
Thrust Tectonics
Publisher
Springer Netherlands
Published
1992
Pages
19-31
DOI
10.1007/978-94-011-3066-0_2
Cited by
85
References
1
Language
en

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