Articles | Volume 12, issue 11
https://doi.org/10.5194/se-12-2479-2021
https://doi.org/10.5194/se-12-2479-2021
Research article
 | 
03 Nov 2021
Research article |  | 03 Nov 2021

Detrital zircon provenance record of the Zagros mountain building from the Neotethys obduction to the Arabia–Eurasia collision, NW Zagros fold–thrust belt, Kurdistan region of Iraq

Renas I. Koshnaw, Fritz Schlunegger, and Daniel F. Stockli

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Subject area: Tectonic plate interactions, magma genesis, and lithosphere deformation at all scales | Editorial team: Structural geology and tectonics, paleoseismology, rock physics, experimental deformation | Discipline: Tectonics
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Cited articles

Abdallah, F. T. and Al-Dulaimi, S. I.: Biostratigraphy of the Upper Cretaceous for selected sections in northern Iraq, Iraqi Journal of Science, 60, 545–553, 2019. 
Abdel-Kireem, M. R.: Planktonic foraminifera and stratigraphy of the Tanjero Formation (Maastrichtian), northeastern Iraq, Micropaleontology, 32, 215–231, 1986. 
Abdollahi, F., Nabatian, G., Li, J. W., Honarmand, M., and Ebrahimi, M.: Saheb Granitoid Batholith, North of Kurdistan: An Evidence of Cretaceous-Paleocene Magmatism in the Sanandaj-Sirjan Zone, Journal Of Economic Geology, 12, 359–376, 2020. 
Abdula, R. A., Chicho, J., Surdashy, A., Nourmohammadi, M. S., Hamad, E., Muhammad, M. M., Smail, A. A., and Ashoor, A.: Sedimentology of the Govanda Formation at Gali Baza locality, Kurdistan region, Iraq, Iraqi Bulletin of Geology and Mining, 14, 1–12, 2018. 
Agard, P., Omrani, J., Jolivet, L., and Mouthereau, F.: Convergence history across Zagros (Iran): constraints from collisional and earlier deformation, Int. J. Earth Sci., 94, 401–419, 2005. 
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Short summary
As continental plates collide, mountain belts grow. This study investigated the provenance of rocks from the northwestern segment of the Zagros mountain belt to unravel the convergence history of the Arabian and Eurasian plates. Provenance data synthesis and field relationships suggest that the Zagros Mountains developed as a result of the oceanic crust emplacement on the Arabian continental plate, followed by the Arabia–Eurasia collision and later uplift of the broader region.