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ESurf | Articles | Volume 7, issue 1
Earth Surf. Dynam., 7, 321–344, 2019
https://doi.org/10.5194/esurf-7-321-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Earth Surf. Dynam., 7, 321–344, 2019
https://doi.org/10.5194/esurf-7-321-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 26 Mar 2019

Research article | 26 Mar 2019

Dating and morpho-stratigraphy of uplifted marine terraces in the Makran subduction zone (Iran)

Raphaël Normand et al.
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Cited articles  
Al-Lazki, A., Al-Damegh, K. S., El-Hadidy, S. Y., Ghods, A., and Tatar, M.: Pn-velocity structure beneath Arabia-Eurasia Zagros collision and Makran subduction zones, Geol. Soc. London Spec. Publ., 392, 45–60, https://doi.org/10.1144/SP392.3, 2014. 
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Arz, H. W., Lamy, F., Ganopolski, A., Nowaczyk, N., and Pätzold, J.: Dominant Northern Hemisphere climate control over millennial-scale glacial sea-level variability, Quat. Sci. Rev., 26, 312–321, https://doi.org/10.1016/j.quascirev.2006.07.016, 2007. 
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We studied and mapped uplifted marine terraces in southern Iran that are part of the Makran subduction zone. Our results show that most exposed terraces were formed in the last 35 000–250 000 years. Based on their altitude and the paleo sea-level, we derive surface uplift rates of 0.05–5 mm yr−1. The marine terraces, tilted with a short wavelength of 20–30 km, indicate a heterogeneous accumulation of deformation in the overriding plate.
We studied and mapped uplifted marine terraces in southern Iran that are part of the Makran...
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