Zagros orogeny: a subduction-dominated process

P Agard, J Omrani, L Jolivet, H Whitechurch… - Geological …, 2011 - cambridge.org
This paper presents a synthetic view of the geodynamic evolution of the Zagros orogen
within the frame of the Arabia–Eurasia collision. The Zagros orogen and the Iranian plateau …

[HTML][HTML] Arabia-Eurasia convergence and collision control on Cenozoic juvenile K-rich magmatism in the South Armenian block, Lesser Caucasus

M Grosjean, R Moritz, H Rezeau, S Hovakimyan… - Earth-Science …, 2022 - Elsevier
Abstract The South Armenian Block (SAB) belongs to the Lesser Caucasus, and it is located
where the Central Tethyan belt bends from an EW orientation in Turkey to the NW-oriented …

Miocene tectono-magmatic events and gold/poly-metal mineralizations in the Takab-Delijan belt, NW Iran

SM Heidari, P Afzal, B Sadeghi - Geochemistry, 2023 - Elsevier
Abstract The Takab-Delijan (TD) magmatic belt in NW Iran is a part of the Zagros orogenic
belt which has imminence with epithermal, porphyry and carlin types of mineralization. This …

Present‐day kinematics and fault slip rates in eastern Iran, derived from 11 years of GPS data

A Walpersdorf, I Manighetti, Z Mousavi… - Journal of …, 2014 - Wiley Online Library
We analyze new GPS data spanning 11 years at 92 stations in eastern Iran. We use these
data to analyze the present‐day kinematics and the slip rates on most seismogenic faults in …

Rheological heterogeneities control the non‐progressive uplift of the young Iranian plateau

Y Gao, L Chen, J Yang, K Wang - Geophysical Research …, 2023 - Wiley Online Library
The Iranian plateau is at the early stage of plateau development and intracontinental
deformation in response to the Arabia‐Eurasia collision. Its compressive deformation is …

Late Cenozoic volcanism and rates of active faulting in eastern Iran

RT Walker, P Gans, MB Allen, J Jackson… - Geophysical Journal …, 2009 - academic.oup.com
Summary We present new 40Ar/39Ar ages of samples of volcanic rock exposed along the
remote margins of the Dasht-e Lut desert in eastern Iran. Close spatial relationships …

Neogene sediments and modern depositional environments of the Zagros foreland basin system

M Pirouz, G Simpson, A Bahroudi, A Azhdari - Geological Magazine, 2011 - cambridge.org
A sedimentological investigation of the Neogene deposits of the Zagros foreland basin in
SW Iran reveals a continuous and largely gradational passage from supratidal and sabkha …

Structural characteristics and formation mechanism of the earth fissures as a geohazard in Birjand, Iran

A Rashidi, MM Khatib, R Derakhshani - Applied Sciences, 2022 - mdpi.com
Earth fissure structures are a common type of geohazard associated with geotechnical
surface ruptures that can occur almost anywhere on the ground surface due to a variety of …

Inherited strike‐slip faults as an origin for basement‐cored uplifts: Example of the Kungey and Zailiskey ranges, northern Tian Shan

J Selander, M Oskin, C Ormukov, K Abdrakhmatov - Tectonics, 2012 - Wiley Online Library
Basement‐cored uplifts bounded by steeply dip** reverse faults are mechanically difficult
to explain. Reactivation of strike‐slip faults that aid the formation of new, high‐angle reverse …

Oroclinal bending, distributed thrust and strike-slip faulting, and the accommodation of Arabia–Eurasia convergence in NE Iran since the Oligocene

J Hollingsworth, M Fattahi, R Walker… - Geophysical Journal …, 2010 - academic.oup.com
Regional shortening is accommodated across NE Iran in response to the collision of Arabia
with Eurasia. We examine how N–S shortening is achieved on major thrust systems …