[PDF][PDF] Brittle tectonics and palaeostress reconstructions in the Zagros: passive palaeo-margin and continental collision
P Navabpour - 2009 - researchgate.net
This dissertation focuses on brittle tectonic evolution of the inner zones of the Zagros fold-
and-thrust belt in the Fars and Kermanshah provinces of Iran. A palaeostress reconstruction�…
and-thrust belt in the Fars and Kermanshah provinces of Iran. A palaeostress reconstruction�…
Stress states in the Zagros fold-and-thrust belt from passive margin to collisional tectonic setting
P Navabpour, E Barrier�- Tectonophysics, 2012 - Elsevier
The present-day Zagros fold-and-thrust belt of SW-Iran corresponds to the former Arabian
passive continental margin of the southern Neo-Tethyan basin since the Permian–Triassic�…
passive continental margin of the southern Neo-Tethyan basin since the Permian–Triassic�…
Mesozoic extensional brittle tectonics of the Arabian passive margin, inverted in the Zagros collision (Iran, interior Fars)
P Navabpour, J Angelier, E Barrier�- Geological Society, London�…, 2010 - lyellcollection.org
The present Zagros mountain belt of SW Iran is known to be the former NE Arabian passive
continental margin of the southern Neo-Tethyan basin, which originated by Permian�…
continental margin of the southern Neo-Tethyan basin, which originated by Permian�…
Cenozoic post-collisional brittle tectonic history and stress reorientation in the High Zagros Belt (Iran, Fars Province)
P Navabpour, J Angelier, E Barrier�- Tectonophysics, 2007 - Elsevier
The Zagros fold-and-thrust belt of SW-Iran is among the youngest continental collision zones
on Earth. Collision is thought to have occurred in the late Oligocene–early Miocene�…
on Earth. Collision is thought to have occurred in the late Oligocene–early Miocene�…
Palaeostress review of the Zagros fold-and thrust belt and tectonic implications
P Navabpour, E Barrier�- EGU General�…, 2011 - meetingorganizer.copernicus.org
The present-day Zagros fold-and-thrust belt of SW-Iran corresponds to the former Arabian
passive continental margin of the southern Neo-Tethyan basin since the Permian–Triassic�…
passive continental margin of the southern Neo-Tethyan basin since the Permian–Triassic�…
Oblique oceanic opening and passive margin irregularity, as inherited in the Zagros fold‐and‐thrust belt
P Navabpour, E Barrier, H McQuillan�- Terra Nova, 2014 - Wiley Online Library
The Zagros fold‐and‐thrust belt of SW Iran represents deformation of the former Arabian
passive margin since Permian–Triassic opening of the Neo‐Tethys ocean. The Zagros belt�…
passive margin since Permian–Triassic opening of the Neo‐Tethys ocean. The Zagros belt�…
Evolution of the stress fields in the Zagros Foreland Folded Belt using focal mechanisms and kinematic analyses: the case of the Fars salient, Iran
K Sarkarinejad, B Zafarmand, B Oveisi�- International Journal of Earth�…, 2018 - Springer
Abstract The NW–SE trending Zagros orogenic belt was initiated during the convergence of
the Afro–Arabian continent and the Iranian microcontinent in the Late Cretaceous. Ongoing�…
the Afro–Arabian continent and the Iranian microcontinent in the Late Cretaceous. Ongoing�…
Brittle tectonic reconstruction of palaeo-extension inherited from Mesozoic rifting in West Zagros (Kermanshah, Iran)
P Navabpour, J Angelier, E Barrier�- Journal of the Geological�…, 2011 - lyellcollection.org
The present-day Zagros mountain belt of SW Iran corresponds to the former Arabian passive
continental margin of the southern Neo-Tethyan basin, which existed since a Permian�…
continental margin of the southern Neo-Tethyan basin, which existed since a Permian�…
Pre-Permian uplift and diffuse extensional deformation in the High Zagros Belt (Iran): integration in the geodynamic evolution of the Arabian plate
S Tavakoli-Shirazi, D Frizon de Lamotte…�- Arabian Journal of�…, 2013 - Springer
Abstract The High Zagros Belt includes exposures of Lower Palaeozoic rocks in the core of
several thrusted anticlines developed during the Cenozoic Zagros orogeny. The structural�…
several thrusted anticlines developed during the Cenozoic Zagros orogeny. The structural�…
Structural variation along the Zagros and the nature of the Dezful Embayment
MB Allen, M Talebian�- Geological magazine, 2011 - cambridge.org
Structure varies along strike in the Zagros fold-and-thrust belt of Iran, which is a principal
element in the Arabia–Eurasia continental collision. Pre-collision, Late Cretaceous ophiolite�…
element in the Arabia–Eurasia continental collision. Pre-collision, Late Cretaceous ophiolite�…