High‐resolution lithospheric structure of the Zagros collision zone and Iranian Plateau

MA Irandoust, K Priestley… - Journal of Geophysical …, 2022 - Wiley Online Library
From a joint analysis of fundamental mode Rayleigh wave group velocities and P‐wave
receiver functions, we derive a new, high‐resolution 3D shear‐wave velocity (Vs) model for …

Determination of the dipping direction of a blind reverse fault from InSAR: case study on the 2017 Sefid Sang earthquake, northeastern Iran

N Ghayournajarkar, Y Fukushima - Earth, Planets and Space, 2020 - Springer
Determining the fault parameters of an earthquake is fundamental for studying the
earthquake physics, understanding the seismotectonics of the region, and forecasting future …

The kinematics of the Dasht-e Bayaz earthquake fault during Pliocene-Quaternary: Implications for the tectonics of eastern Central Iran

F Baniadam, E Shabanian, O Bellier - Tectonophysics, 2019 - Elsevier
Abstract The Arabia-Eurasia convergence is accommodated across the Iranian plateau and
surrounding mountain ranges. Strike-slip faults play significant roles in the current …

Evolution of the stress field at the junction of Talesh–Alborz–Central Iran during the past 5 Ma: implications for the tectonics of NW Iran

M Aflaki, E Shabanian, S Sahami, M Arshadi - Tectonophysics, 2021 - Elsevier
Tectonic stresses governed by the Arabia–Central Iran collision are transferred throughout
the Iranian Plateau. The orientation of the maximum horizontal stress (σ 1) significantly …

[HTML][HTML] 影像大地测量技术再探伊朗桑塞菲德2017年MW6.1地震盲断层倾向

周成, 马张烽, 蒋弥 - 地球物理学报, 2021 - html.rhhz.net
在盲断层参数未知的情况下, 确定断层模型参数是获取震源机制的基础, 也是地震风险性分析的
首要任务. 2017 年伊朗桑塞菲德MW 6.1 地震倾角的确定作为盲断层参数确定的一个宝贵实例 …

Permian to recent tectonic evolution of the Palaeotethys suture zone in NE Iran

M Ershadinia, F Ghaemi, SM Homam - Journal of Asian Earth Sciences, 2023 - Elsevier
Abstract The Fariman Complex in northeastern Iran plays an important role in deciphering
the geodynamic evolution of Palaeotethys and the Cimmerian orogeny in Central Asia. The …

Re-exploration of fault dipping direction in Iran Sang sefid 2017 MW6.1 earthquake using imaging geodesy

C ZHOU, ZF MA, M JIANG - Chinese Journal of Geophysics, 2021 - en.dzkx.org
The first step of earthquake risk analysis is to determine the blind fault parameters. There are
many disputes about the parameter determination of each blind fault. In this paper, we took …

Co-seismic deformation and slip distribution of 5 April 2017 Mashhad, Iran earthquake using InSAR sentinel-1A image: implication to source characterization and …

SK Prajapati, OP Mishra - Natural Hazards, 2021 - Springer
We analyzed interferometric synthetic aperture radar sentinel-1A-based observations to
characterize the source of 5 April 2017 Mashhad, Iran mainshock (Mw 6.1), for the first time …

A major medieval earthquake on the main Köpetdag (Kopeh Dagh) Fault, Turkmenistan

N Dodds, G Begenjev, Y Bezmenov… - Bulletin of the …, 2022 - pubs.geoscienceworld.org
The Main Köpetdag fault (MKDF) of Turkmenistan is one of the longest (≈ 500 km) and the
most rapidly straining (9.1±1.3 mm/yr) faults of the Arabia–Eurasia collision zone, and yet, in …

Interaction between the far-field stress and crustal boundary faults in the kinematics of active deformation around the Lut Block, Eastern Iran

M Aflaki, Z Mousavi - Tectonophysics, 2021 - Elsevier
We investigate the effects of far-field stresses and major crustal boundary faults in the
deviation of local stresses around the Lut Block of the southeastern Iranian plateau in the …