Articles | Volume 7, issue 2
https://doi.org/10.5194/se-7-659-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-7-659-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Spatial evolution of Zagros collision zone in Kurdistan, NW Iran: constraints on Arabia–Eurasia oblique convergence
Shahriar Sadeghi
Department of Geology, Tarbiat Modares University, Tehran, Iran
Ali Yassaghi
CORRESPONDING AUTHOR
Department of Geology, Tarbiat Modares University, Tehran, Iran
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32 citations as recorded by crossref.
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- Post-Cretaceous structural reconstruction of the west Central Iranian micro-plate: Insights from structural and magnetic fabrics (AMS) constraints M. Tadayon et al. 10.1016/j.jsg.2022.104601
- Extraction of Lineaments Using Landsat Image and Digital Elevation Model: A Case Study of Zagros Orogenic Belt, West Iran S. Sadeghi et al. 10.1007/s12524-024-01956-5
- Tectonic evolution of the Zagros foreland basin since Early Cretaceous, SW Iran: Regional tectonic implications from subsidence analysis H. Karimnejad Lalami et al. 10.1016/j.jseaes.2020.104550
- Early Cretaceous sedimentary provenance and structural evolution of the central Sanandaj–Sirjan Zone, Iran: implications for palaeogeographic reconstructions of the northern Neo-Tethyan margin M. Salehi & M. Tadayon 10.1080/00206814.2019.1647120
- The Tethyan Seaway during the early to middle Miocene – New data and a review W. Piller et al. 10.1016/j.gr.2024.08.004
- Earthquake-Induced Ground Deformation Assessment via Sentinel-1 Radar Aided at Darbandikhan Town F. Saed et al. 10.1155/2022/2020069
- Structural assessment of the Bradost and Berat structures in Imbricate and High Folded zones—Iraqi Kurdistan Zagros belt H. Balaki & A. Omar 10.1007/s12517-019-4251-1
- STRUCTURAL STYLE AND TIMING OF NW‐SE TRENDING ZAGROS FOLDS IN SW IRAN: INTERACTION WITH NORTH‐SOUTH TRENDING ARABIAN FOLDS AND IMPLICATIONS FOR PETROLEUM GEOLOGY J. Vergés et al. 10.1111/jpg.12850
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- Experimental deformation partitioning in obliquely converging orogens with lateral variations of basal décollement rheology: Inferences for NW Zagros, Iran S. Sadeghi et al. 10.1016/j.tecto.2016.05.014
- Impulsive Source of the 2017 MW=7.3 Ezgeleh, Iran, Earthquake B. Gombert et al. 10.1029/2018GL081794
- Seismic potential on the northwestern Main Recent Fault (Iran) revealed by InSAR J. Hu & Y. Yang 10.1016/j.procs.2024.06.434
- The 12 November 2017 Mw 7.3 Ezgeleh‐Sarpolzahab (Iran) Earthquake and Active Tectonics of the Lurestan Arc E. Nissen et al. 10.1029/2018JB016221
- Effect of tectonic-climatic controllers on the transition of Endorheic to Exorheic Basins in the Zagros mountain range G. Hassan Jafari et al. 10.1007/s11629-023-8328-7
- Midcrustal Thrusting and Vertical Deformation Partitioning Constraint by 2017 Mw 7.3 Sarpol Zahab Earthquake in Zagros Mountain Belt, Iran Y. Yang et al. 10.1785/0220180022
- Ramp-Flat and Splay Faulting Illuminated by Frictional Afterslip Following the 2017 Mw 7.3 Sarpol-e Zahab Earthquake Z. Guo et al. 10.1785/0220230425
- Early Jurassic Rifting of the Arabian Passive Continental Margin of the Neo‐Tethys. Field Evidence From the Lurestan Region of the Zagros Fold‐and‐Thrust Belt, Iran S. Tavani et al. 10.1029/2018TC005192
- Geodetic Constraints of the 2017 Mw7.3 Sarpol Zahab, Iran Earthquake, and Its Implications on the Structure and Mechanics of the Northwest Zagros Thrust‐Fold Belt W. Feng et al. 10.1029/2018GL078577
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- Depth‐Varying Friction on a Ramp‐Flat Fault Illuminated by ∼3‐Year InSAR Observations Following the 2017 Mw 7.3 Sarpol‐e Zahab Earthquake Z. Guo et al. 10.1029/2022JB025148
- Timing of the Arabia-Eurasia continental collision—Evidence from detrital zircon U-Pb geochronology of the Red Bed Series strata of the northwest Zagros hinterland, Kurdistan region of Iraq R. Koshnaw et al. 10.1130/G45499.1
- A Review: The Tectonic Perspective and seismic response of Darbandikhan Dam Stability and potential solutions K. Mahdi 10.1088/1755-1315/790/1/012018
- Lineament Extraction via Satellite Imagery for a Seismic Zone in the Sarpol Zahab Region R. Ali et al. 10.1007/s41976-024-00148-6
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- Strain Geometry and Vorticity Analysis of the Deformed Radiolarian Rocks in the Abade-Tashk Area, the Zagros Suture Zone, Iran R. Tavakkoli et al. 10.1007/s12583-021-1606-9
- The Meso-Cenozoic fracture pattern of the Lurestan region, Iran: The role of rifting, convergence, and differential compaction in the development of pre-orogenic oblique fractures in the Zagros Belt S. Tavani et al. 10.1016/j.tecto.2018.10.031
- Geothermal Model of the Shallow Crustal Structure across the “Mountain Front Fault” in Western Lurestan, Zagros Thrust Belt, Iran M. Basilici et al. 10.3390/geosciences9070301
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Short summary
Detailed field investigations, a crustal-scale cross section and stratigraphic data are used to document oblique convergence in Kurdistan, NW Zagros. Two stages of deformation partitioning are recognized in the external part of Zagros, one in the Late Cretaceous by obduction and the other in the Cenozoic by collision. Thus, it is proposed that oblique convergence of Arabian and Eurasian plates in Zagros initiated in the Late Cretaceous, consistent with global plate reconstructions.
Detailed field investigations, a crustal-scale cross section and stratigraphic data are used to...