SEARCH

SEARCH BY CITATION

References

  • Basilevsky, A. T., and J. W. Head (2000), Geologic units on Venus: Evidence for their global correlation, Planet. Space Sci., 48, 75111.
  • Berthé, D., P. Choukroune, and P. Jegouzo (1979), Orthogneiss, mylonite and non coaxial deformation of granites: The example of the South American Shear Zone, J. Struct. Geol., 1, 3142.
  • Brown, C. D., and R. E. Grimm (1999), Recent tectonic and lithospheric thermal evolution of Venus, Icarus, 139, 4048.
  • Carreras, J. (1997), Shear zones in foliated rocks: Geometry and kinematics, in Evolution of Geological Structures in Micro- to Macro-scales, edited by S. Sengupta, pp. 185201, CRC Press, Boca Raton, Fla.
  • Corsini, M., A. Vauchez, and R. Caby (1996), Ductile duplexing at a bend of a continental-scale strike-slip shear zone: Example from Brazil, J. Struct. Geol., 18, 385394.
  • Destro, N., P. Szatmari, and E. A. Ladeira (1994), Post-Devonian transpressional reactivation of a Proterozoic ductile shear zone in Ceara, NE Brazil, J. Struct. Geol., 16, 3545.
  • Ebert, H. D., F. Chemale Jr., M. Babinski, A. C. Artur, and W. R. Van Schumus (1996), Tectonic setting and U/Pb zircon dating of the transpressive Rio Paraiba do Sul Shear Belt, SE Brazil, Tectonics, 15, 688699.
  • Farr, T. G. (1993), Radar interaction with geological surfaces, in Guide to Magellan Image Interpretation, edited by J. P. Ford et al., pp. 4556, Jet Propul. Lab., Pasadena, Calif.
  • Ford, J. P., R. G. Blom, J. A. Crisp, C. Elach, T. G. Farr, R. S. Saunders, E. E. Theiug, S. D. Wall, and S. B. Yewell (1989), Spaceborne Radar Observations—A Guide for Radar-Image Analysis, Jet Propul. Lab., Pasadena, Calif.
  • Ghail, R. C. (2002), Structure and evolution of southeast Thetis Regio, J. Geophys. Res., 107(E8), 5060, doi:10.1029/2001JE001514.
  • Ghent, R., and V. L. Hansen (1999), Structural and kinematic analysis of eastern Ovda Regio, Venus: Implications for crustal plateau formation, Icarus, 139, 116136.
  • Gilmore, M. S., G. C. Collins, M. A. Ivanov, L. Marinangeli, and J. W. Head (1998), Styles and sequence of extensional structures in tessera terrain, Venus, J. Geophys. Res., 103, 16,81316,840.
  • Hanmer, S. (1988), Great Slave Lake Shear Zone, Canadian Shield: Reconstructed vertical profile of a crustal-scale fault zone, Tectonophysics, 149, 245264.
  • Hansen, V. L. (1992), Regional non-coaxial deformation on Venus: Evidence from western Itzapapalotl tessera, Lunar Planet. Sci., XXIII, 479480.
  • Hansen, V. L., and J. A. Willis (1996), Structural analysis of a sampling of Tesserae: Implications for Venus geodynamics, Icarus, 123, 296312.
  • Hansen, V. L., R. J. Phillips, J. J. Willis, and R. R. Ghent (2000), Structures in tesserae terrain, Venus: Issues and answers, J. Geophys. Res., 105, 41354152.
  • Head, J. W., and A. T. Basilevsky (1998), Sequence of tectonic deformation in the history of Venus: Evidence from global stratigraphic relations, Geology, 26, 3538.
  • Hippertt, J. (1999), Are S–C structures, duplexes and conjugate shear zones different manifestations of the same scale-invariant phenomenon? J. Struct. Geol., 21, 975984.
  • Ivanov, M. A., and J. W. Head (1996), Tesserae terrain on Venus: A survey of the global distribution, characteristics and relation to surrounding units from Magellan data, J. Geophys. Res., 101, 14,86114,908.
  • Koenig, E., and A. Aydin (1998), Evidence for large-scale strike-slip faulting on Venus, Geology, 26, 551554.
  • Lin, A. (1999), S–C cataclasite in granitic rock, Tectonophysics, 304, 257273.
  • Lin, A. (2001), S–C fabrics developed in cataclastic rocks from the Nojima fault zone, Japan and their implications for tectonic history, J. Struct. Geol., 23, 11671178.
  • Lister, G. S., and A. W. Snoke (1984), S–C mylonites, J. Struct. Geol., 6, 617638.
  • Nimmo, F., and D. McKenzie (1998), Volcanism and tectonics on Venus, Annu. Rev. Earth Planet. Sci., 26, 2351.
  • Passchier, C. W., and R. A. J. Trouw (1997), Microtectonics, 289 pp., Springer, New York.
  • Pritchard, M. E., V. L. Hansen, and J. J. Willis (1997), Structural evolution of western Fortuna tesserae, Venus, Geophys. Res. Lett., 24, 23392342.
  • Ramsay, J. G. (1980), Shear zone geometry, J. Struct. Geol., 2, 8399.
  • Ramsay, J. G., and R. J. Listle (2000), The Techniques of Modern Structural Geology, vol. 3, 361 pp., Elsevier, New York.
  • Ranalli, G. (1995), Rheology of the Earth, 2nd ed., 413 pp., Chapman and Hall, CRC Press, Boca Raton, Fla.
  • Romeo, I., R. Capote, and F. Anguita (2005), Tectonic and kinematic study of a strike-slip zone along the southern margin of Central Ovda Regio, Venus: Geodynamical implications for crustal plateaux formation and evolution, Icarus, 175, 320334.
  • Shimamoto, T. (1989), The origin of S–C mylonites and a new fault-zone model, J. Struct. Geol., 11, 5164.
  • Solomon, S. C., J. W. Head, W. M. Kaula, D. McKenzie, B. Parsons, R. J. Phillips, G. Schubert, and M. Talwani (1991), Venus tectonics: Initial analysis from Magellan, Science, 252, 297312.
  • Tanaka, K. L., et al. (1994), The Venus Geologic Mappers' Handbook, 2nd ed., 52 pp., U.S. Geol. Surv. Open File Rep., 94-438.
  • Tuckwell, G. W., and R. C. Ghail (2003), A 400-km-scale strike-slip zone near the boundary of Thetis Regio, Venus, Earth Planet. Sci. Lett., 211, 4555.
  • Turcottle, D. L., and G. Schubert (2002), Geodynamics, 2nd ed., 436 pp., Cambridge Univ. Press, New York.
  • Vauchez, A., and M. Egydio-Silva (1992), Termination of a continental-scale strike-slip fault in partially melted crust: The West-Pernambuco shear zone, northeast Brazil, Geology, 20, 10071010.
  • Vauchez, A., S. Pacheco-Neves, R. Caby, M. Corsini, M. Egydio-Silva, M. Arthaud, and V. Amaro (1995), The Borborema shear zone system, J. South Am. Earth Sci., 8, 247266.
  • Woodcock, N. H., and M. Fischer (1986), Strike-slip duplexing, J. Struct. Geol., 8, 725735.