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'''Strain partitioning''' is commonly referred to as a [[Deformation (engineering)|deformation]] process in which the total [[Deformation (mechanics)|strain]] experienced on a rock, area, or region, is heterogeneously distributed in-terms of the strain intensity and strain type (i.e. [[Shear (geology)|pure shear]], [[simple shear]], [[dilation (geology)|dilatation]]).<ref name=Jones&Tanner>Jones, Richard; Tanner, P.W. Geoff (1995). "Strain partitioning in transpression zones". Journal of Structural Geology 17 (6): 793–802.</ref><ref name=Carreras>Carreras, Jordi; Cosgrove, John; Druguet, Elena (2013). "Strain partitioning in banded and/or anisotropic rocks: Implications for inferring tectonic regimes". Journal of Structural Geology 50: 7–21. doi:10.1016/j.jsg.2012.12.003.</ref><ref name=Fossen>Fossen, Haakon (2012). Structural Geology. New York, USA: Cambridge University Press. ISBN 978-0-521-51664-8.</ref> This process is observed on a range of scales spanning from the grain - [[crystal]] scale to the [[tectonic plate|plate]] - lithospheric scale and occurs in both the brittle and plastic deformation regimes.<ref name=Jones&Tanner /><ref name=Carreras /> The manner and intensity by which strain is distributed is controlled by a number of factors listed below.<ref name=Carreras />

'''Strain partitioning''' is commonly referred to as a [[Deformation (engineering)|deformation]] process in which the total [[Deformation (mechanics)|strain]] experienced on a rock, area, or region, is heterogeneously distributed in-terms of the strain intensity and strain type (i.e. [[Shear (geology)|pure shear]], [[simple shear]], [[dilation (geology)|dilatation]]).<ref name=Jones&Tanner>Jones, Richard; Tanner, P.W. Geoff (1995). "Strain partitioning in transpression zones". Journal of Structural Geology 17 (6): 793–802.</ref><ref name=Carreras>Carreras, Jordi; Cosgrove, John; Druguet, Elena (2013). "Strain partitioning in banded and/or anisotropic rocks: Implications for inferring tectonic regimes". Journal of Structural Geology 50: 7–21. doi:10.1016/j.jsg.2012.12.003.</ref><ref name=Fossen>Fossen, Haakon (2012). Structural Geology. New York, USA: Cambridge University Press. ISBN 978-0-521-51664-8.</ref> This process is observed on a range of scales spanning from the grain - [[crystal]] scale to the [[tectonic plate|plate]] - lithospheric scale and occurs in both the brittle and plastic deformation regimes.<ref name=Jones&Tanner /><ref name=Carreras /> The manner and intensity by which strain is distributed is controlled by a number of factors listed below.<ref name=Carreras />