Doming along the Zagros transpression zone, SW Iran: insights from microstructural analysis of heterogeneous deformation
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences,General Environmental Science
Link
https://link.springer.com/content/pdf/10.1007/s12517-021-06835-8.pdf
Reference141 articles.
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2. Al-Saleh AM, Kassem OM (2012) Microstructural finite strain analysis and 40Ar/39Ar evidence for the origin of the Mizil gneiss dome, eastern Arabian Shield, Saudi Arabia. J Afr Earth Sci 70:24–35. https://doi.org/10.1016/j.jafrearsci.2012.05.004
3. Andresen A, Augland LE, Boghdady GY, Lundmark AM, Elnady OM, Hassan MA, El-Rus MA (2010) Structural constraints on the evolution of the Meatiq gneiss dome (Egypt), East-African Orogen. J Afr Earth Sci 57(5):413–422. https://doi.org/10.1016/j.jafrearsci.2009.11.007
4. Bailey CM, Francis BE, Farnhey EE (2004) Strain and vorticity analysis of transpres- sional high-strain zones from the Virginia Piedmont, USA. In: ALSOP, G. I., Holdsworth, R.E., Mccaffrey, K.J.W., Hand, M. (eds) Flow Processes in Faults and Shear Zones. https://doi.org/10.1144/GSL.SP.2004.224.01.16
5. Barnichon JD, Havenith H, Hoffer B, Charlier R, Jongmans D, Duchesne JC (1999) The deformation of the Egersund-Ogna anorthosite massif, South Norway; finite-element modelling of diapirism. Tectonophysics 303:109–130. https://doi.org/10.1016/S0040-1951(98)00247-9
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