Abstract
In shear zones developed across foliated rocks the relationships between geometry, strain patterns and kinematics differ from those in isotropic rocks. These differences refer to:
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1.
the variability of the existing angle formed by the shear direction and the bent axis of the foliation, a fact that can originate equivocal kinematic inferences; and
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2.
the deviation of this type of shear zones from the heterogeneous simple shear model, caused by the non-passive behaviour of the previous foliation.
In addition to this second point, the presence of a pre-existing foliation induces the development of minor structures arising from buckling instabilities formed at the marginal domains. These questions are reviewed and illustrated with examples taken from the Cap de Creus in the Hercynian basement of the easternmost Pyrenees.
Acknowledgements: Part of this work was developed at the Department of Earth and Planetary Sciences, Johns Hopkins University (Baltimore) with financial support of the DGCICYT (Spain). The work was completed with the financial support of the DGCICYT PB 91-0477 Project. This contribution benefited from the constructive comments of S. Sengupta and from careful review by J. Cosgrove.
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References
Bell, T.H. (1978) Progressive deformation and reorientation of fold axes in a ductile mylonite zone: the Woodroffe thrust. Tectonophysics, 44, 285–320.
Berthé, D., Choukroune, P. and Jegouzo, P. (1979) Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican shear zone. Journal of Structural Geology, 1, 31–42.
Biot, M.A. (1961) Theory of folding of stratified viscoelastic media and its implications in tectonics and orogenesis. Bulletin of the Geological Society of America, 72, 1595–1620.
Bobyarchick, A.R. (1986) The eigenvalues of steady state flow in Mohr space. Tectonophysics, 122 35–51.
Carreras, J. (1975) Determinatión de las relaciones ángulares y de la deformatión por cizalla, para cizallamientos en materiales con una heterogeneidad planar. Acta geol. Hisp., 10, 141–145.
Carreras, J. and Casas, J.M. (1987) On folding and shear zone development: a mesoscale structural study on the transition between two different tectonic styles. Tectonophysics, 135, 87–98.
Carreras, J. and Druguet, E. (1994) Structural zonation as a result of inhomogeneous non-coaxial deformation and its control of syntectonic intrusions: an example from the Cap de Creus area (eastern-Pyrenees). Journal of Structural Geology, 16, 1525–1534.
Carreras, J. and Garcia Celma, A. (1982) Quartz c-axis fabric variation at the margins of a shear zone developed in schists from Cap de Creus (Spain). Acta geol. Hisp., 17, 137–149.
Carreras, J. and Ortuño, F. (1990) Fundamento geométrico y cinemático de la modelización teórica y experimental de deformaciones no-coaxiales. Acta geol. Hisp., 25, 237–259.
Carreras, J., Estrada, A. and White, S. (1977) The effects of folding on the c-axis fabrics of a quartz-mylonite. Tectonophysics, 39, 3–24.
Cobbold, P.R., Cosgrove, J.W. and Summers, J.M.S. (1971) The development of internal structures in deformed anisotropic rocks. Tectonophysics, 12, 23–53.
Cosgrove, J.W. (1976) The formation of crenulation cleavage. Journal of the Geological Society, London, 132, 155–178.
Cosgrove, J.W. (1989) Cleavage, folding and the finite strain ellipsoid. Proceedings of the Geological Association, 100, 461–479.
De Paor, D.G. (1983) Orthographic analysis of geological structures.-I. Deformation theory. Journal of Structural Geology, 5, 255–277.
Escher, A., Escher, J. C. and Warterson, J. (1975) The reorientation of the Kangamiut dyke swarm, West Greenland. Canadian Journal of Earth Sciences, 12, 158, 173.
Flinn, D. (1962) On folding during three-dimensional progressive deformation. Journal of the Geological Society, London, 118, 385–433.
Ghosh, S.K. (1968) Experiments of buckling of multilayers which permit interlayer gliding. Tectonophysics, 6, 207–250.
Ghosh, S.K. and Sengupta, S. (1984) Successive development of plane noncylindrical folds in progressive deformation. Journal of Structural Geology, 6, 703–709.
Ghosh, S.K. and Sengupta, S. (1987) Progressive development of structures in a ductile shear zone. Journal of Structural Geology, 9, 277–286.
Latham, J.P. (1985) A numerical investigation and geological discussion of the relationship between folding, kinking and faulting. Journal of Structural Geology, 7, 237–249.
Lister, G.S. and Williams, P.F. (1983) The partitioning of deformation in flowing rock masses. Tectonophysics, 92, 1–33.
Passchier, C.W., Myers, J.S. and Kröner, A. (1990) Field Geology of High-Grade Gneiss Terrains, Springer-Verlag, Heidelberg.
Platt, J.P. (1984) Secondary cleavages in ductile shear zones. Journal of Structural Geology, 6, 439–442.
Ramberg, H. (1964) Selective buckling of composite layers with contrasted rheological properties. A theory for simultaneous formation of several orders of folds. Tectonophysics, 1, 307–341.
Ramberg, H. and Ghosh, S.K. (1977) Rotation and strain of linear and planar structures in threedimensional progressive deformation. Tectonophysics, 40, 309–357.
Ramsay, J.G. (1967) Folding and fracturing of rocks, McGraw Hill, New York.
Ramsay, J.G. (1980) shear zone geometry: a review. Journal of Structural Geology, 2, 83–99.
Ramsay, J.G. and Allison, I. (1979) Structural analysis of shear zones in an Alpinised Hercynian granite. Schweiz. miner. petrogr. Mitt., 59, 251–279.
Ramsay, J.G. and Graham, R.D. (1970) Strain variations in shear belts. Canadian Journal of Earth Sciences, 7, 786–813.
Ramsay, J.G. and Huber, M.I. (1987) The techniques of structural geology, vol. 2: folds and fractures, Academic Press, London.
Sanderson, D.J. (1973) The development of fold axes oblique to the regional trend. Tectonophysics, 16, 55–70.
Sibson, R.H. (1977) Fault rocks and fault mechanisms. Journal of the Geological Society, London, 133, 191–213.
Simpson, C, Carreras, J. and Losantos, M. (1982) Inhomogeneous deformation in Roses granodiorite. Acta geol. Hisp., 17, 219–226.
Simpson, C. and De Paor, D.G. (1993) Strain and kinematic analysis in general shear zones. Journal of Structural Geology, 15, 1–20.
Skjernaa, L. (1980) Rotation and deformation of randomly oriented planar and linear structures in progressive simple shear. Journal of Structural Geology, 2, 101–109.
Treagus, J.E. and Treagus, S.H. (1981) Folds and the strain ellipsoid: a general model. Journal of Structural Geology, 3, 1–17.
Wheeler, J. (1987) The determination of true shear sense from the deflection of passive markers in shear zones. Journal of the Geological Society, London, 144, 73–77.
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Carreras, J. (1997). Shear zones in foliated rocks: geometry and kinematics. In: Sengupta, S. (eds) Evolution of Geological Structures in Micro- to Macro-scales. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-5870-1_11
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DOI: https://doi.org/10.1007/978-94-011-5870-1_11
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