Fan morphology evidence on Late Quaternary deformation in the southern front of the Central and Eastern Alborz Mountains in the Eyvanekey, Garmsar, Semnan areas, Northern Iran
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/s12517-020-05979-3.pdf
Reference106 articles.
1. Agard P, Omrani J, Jolivet L, Mouthereau F (2005) Convergence history across Zagros (Iran): constraints from collisional and earlier deformation. Int J Earth Sci 94:401–419. https://doi.org/10.1007/s00531-005-0481-4
2. Aghanabati A, Hamedi AR (1994) Geological survey of Iran, Semnan sheet 1:250000
3. Alavi M (1996) Tectonostratigraphic synthesis and structural style of the Alborz Mountain system in Northern Iran. J Geodyn 21:1–33
4. Allen MB, Armstrong HA (2008) Arabia-Eurasia collision and the forcing of mid-Cenozoic global cooling. Palaeogeogr Palaeoclimatol Palaeoecol 265(1-2):52–58. https://doi.org/10.1016/j.palaeo.2008.04.021
5. Allen M, Ghassemi MR, Shahrabi M, Qoashi M (2003) Accommodation of late Cenozoic oblique shortening in the Alborz range, Northern Iran. J Struct Geol 25:659–672. https://doi.org/10.1016/S0191-8141(02)00064-0
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