Jiang D, Williams P F. High-strain zones:A unified model[J]. Journal of Structural Geology, 1998, 20:1105-1120.
[2]
Jiang D, Lin S, Williams P F. Deformation path in highstrain zones, with reference to slip partitioning in transpressional plateboundary regions[J]. Journal of Structural Geology, 2001, 23:991-1005.
[3]
Lin S, Jiang D. Using along-strike variation in strain and kinematics to define the movement direction of curved transpressional shear zones: an example from northwestern Superior Province, Manitoba[J]. Geology, 2001, 29:767-770.
[4]
Lin S, Williams P F. The geometrical relationship between the stretching lineation and the movement direction of shear zones[J].Journal of Structural Geology, 1992, 14:491-497.
[5]
Sanderson D J, Marchini W R D. Transpression[J]. Journal of Structural Geology, 1982, 6:449-458.
[6]
Fossen H, Tikoff B. The deformation matrix for simultaneous simple shearing, pure shearing and volume change, and its application to transpression-transtension tectonics[J]. Journal of Strucrural Geology, 1993, 15:413-422.
[7]
Fossen H, Tikoff B, Teyssier C. Strain modeling of transpressional and transtensional deformation[J]. Norsk Geologisk Tidsskrift, 1994, 74:134-145.
[8]
Jones R R, Holdsworth R E, Baily W. Lateral extrusion in transpression zones[J]. Journal of Structural Geology, 1997, 19: 1201-1217.
[9]
Fossen H, Tikoff B. Extended models of transpression and transtension, and application to tectonic settings[C]//Holdsworth R E, Strachan R, Dewey J.Continental Transpressional and Transtensional Tectonics. Geological Society Special Publication, 1998, 135:15-33.
[10]
Tikoff B, Fossen H. Three-dimensional reference deformations and strain facies[J]. Journal of Structural Geology, 1999, 21: 1497-1521.
[11]
Passchier C W. Monodinic model shear zones[J]. Journal of Structural Geology, 1998, 20:1121-1137.
[12]
Hudleston P J, Schultz-Ela D, Southwick D L. Transpression in an Archean greenstone belt, northern Minnesota[J]. Canadian Journal of Earth Sciences, 1988, 25:1060-1068.
[13]
Lin S. The stratigraphy and structural geology of the southeastern Cape Breton Highlands National Park and its implications for the tectonic evolution of Cape Breton Island, Nova Scotia,with emphasis on lineations in shear zones[D]. PhD thesis, the University of New Brunswick, Fredericton, Canada, 1992.
[14]
Goodwin L B, Williams P F. Deformation path partitioning within a transpressive shear zone, Marble Cove, Newfoundland [J]. Journal of Structural Geology, 1996, 18:975-990.
[15]
Dutton B J. Finite strains in transpression zones with no boundary slip[J]. Journal of Structural Geology, 1997, 19:1189-1200.
[16]
Jones R R, Tanner P W G. Strain partitioning in transpression zones[J]. Journal of Structural Geology, 1995, 17:793-802.
[17]
Lin S, Jiang D, Williams P F. Importance of differentiating ductile slickenside striations from stretching lineations and variation of shear direction across a high-strain zone[J]. Journal of Structural Geology, 1997, 29:850-862.
[18]
Czeck D M, Hudleston P J. Testing models for obliquely plunging lineations in transpression: a natural example and theoretical discussion[J]. Journal of Structural Geology, 2003, 25:959-982.
[19]
Czeck D M, Hudleston P J. Physical experiments of vertical transpression with localized, nonvertical extrusion [J]. Journal of Structural Geology, 2004, 26:573-581.
[20]
Wellman H W. New Zealand Quaternary tectonics[J]. Geologisches Rundschan, 1955, 43:248-257.
[21]
Walcott R I. Modes of oblique compression: Late Cenozoic tectonics of the South Island of New Zealand [J]. Reviews of Geophysics, 1998, 36 : 1-26.
[22]
Cooper A F, Norris R J. Anatomy, structural evolution and slip rate of a plate boundary thrust: the Alpine Fault at Gaunt Creek, Westland, New Zealand[J]. Geological Society of America Bulletin, 1994, 106:627-633.
[23]
Norris R J, Cooper A F. Origin of small-scale segmentation and transpressional thrusting at the Alpine fault, New Zealand[J]. Bulletin of the Geological Society of America, 1995, 107:231- 240.
[24]
Norris R J, Koons P O, Cooper A F. The obliquely-convergent phte boundary in the South Island of New Zealand: implications for ancient collision zones[J]. Journal of Structural Geology, 1990, 12:715-725.
[25]
Norris R J, Cooper A F. Erosional control on the structural evolution of a transpressional thrust complex on the Alpine fault, New Zealand[J]. Journal of Structural Geology, 1997,19:1323-1342.
[26]
Sibson R H, White S H, Atkinson B K. Fault rock distribution and structure within the Alpine fault zone: a preliminary report[J]. Royal Society of New Zealand Bulletin, 1979, 18:55-65.
[27]
Williams P F, Jiang D, Lin S. Interpretation of deformation fabrics of infrastructure zone rocks in the context of channel flow and other tectonic models[C]//Law K, Searle M, Godin L. Channel Flow, Ductile Extrusion and Exhumation of Lower-mid Crust in Continental Collision Zones. Geological Society Special Publications, 2006, 268:221-235.
[28]
Williams P F, Vernon P, H. Origin of a vertical lineation in conjugate transcurrent shear-zones at Broken Hill, Australia[J]. Tectonophysics, 2001, 335:163-182.
[29]
Bilby B A, Eshelby J D, Kundu A K. The change of shape of a viscous ellipsoidal region embedded in a slowly deforming matrix having a different viscosity [J]. Tectonophysics, 1975,28:265-274.
[30]
Bilby B A, Kolbuszewski M L. The finite deformation of an inhomogeneity in two-dimensional slow viscous incompressible flow[J]. Proceedings of the Royal Society of London, 1977,A355:335-353.
[31]
Jiang D. Numerical modeling of the motion of rigid ellipsoidal objects in slow viscous flows: a new approach[J]. Journal of Structural Geology, 2007, 29:189-200.
[32]
Jiang D. Numerical modeling of the motion of deformable ellipsoidal objects in slow viscous flows [J]. Journal of Structural Geology, 2007, 29:435-452.
[33]
Berthe D, Choukroune P, Jegouzo P. Orthogneiss, mylonite and non coaxial deformation of granite: the example of the South Armorican shear zone [J]. Journal of Structural Geology,1979, 1:31-42.
[34]
Lister G S, Snoke A W. S-C mylonites[J]. Journal of Structural Geology, 1984, 6:617-638.
[35]
Lin S, Williams P F. The origin of ridge-in-groove slickenside striae and associated steps in an S-C mylonite [J]. Journal of Structural Geology, 1992, 14:315-321.
[36]
Means W D. The concept of steady state foliation[J]. Tectonophysics, 1981, 78:179-199.
[37]
Ramsay J G, Graham R H. Strain variation in shear belts[J]. Canadian Journal of Earth Sciences, 1970, 7:786-813.
[38]
Ramsay J G. Shear zone geometry: a review[J]. Journal of Structural Geology, 1980, 2:83-89.
[39]
Robin P-Y F, Cruden A R. Strain and vorticity patterns in ideally ductile transpressional zones[J]. Journal of Structural Geoloby, 1994, 16:447-466.
[40]
Lin S, Jiang D, Williams P F. Transpression (or transtension) zones of triclinic symmetry: natural example and theoretical modeling[C]//Holdsworth R E, Strachran R A, Dewey J F. Continental Transpressional and Transtensional Tectonics. Geological Society Special Publications, 1998, 135:41-57.
[41]
Tikoff B, Greene D. Stretching lineations in transpressional shear zones: An example from the Sierra Nevada Batholith, California[J]. Journal of Structural Geology, 1997, 19:29-39.
[42]
Jiang D. Problems with transpression and transtension[C]//Geological Association of Canada-Mineral Association of Canada Abstracts. 2005, 30:97.
[43]
Tikoff B, Teyssier C. Strain modeling of displacement-field partitioning in transpressional orogens[J]. Journal of Structural Geology, 1994, 16:1575-1588.
[44]
Kuiper Y D, Jiang D, Lin S. Relationship between non-cylindrical fold geometry and the shear direction in monoclinic and triclinic shear zones[J]. Journal of Structural Geology, 2007, 29: 1022 - 1033.
[45]
Jeffery G B. The motion of ellipsoidal particles immersed in a viscous fluid[J]. Proceedings of the Royal Society of London, 1922, A102:161-179.
[46]
Jeffery G B. The motion of ellipsoidal particles immersed in a viscous fluid[J]. Proceedings of the Royal Society of London, 1922, A102:161-179.
[47]
Eshelby J D. The elastic field outside an ellipsoidal inclusion[J]. Proceedings of the Royal society of London, 1959, A252:561- 569.
