Geologic history of the Sabzevar oceanic Basin, NE Iran: An overview from continental rifting to obduction in the NeoTethys oceanic system
The issue about the Sabzevar Oceanic Basin (SOB) lifetime and its paleogeographic
position, as a branch of the NeoTethyan oceanic system in Northeast Iran, has long been …
position, as a branch of the NeoTethyan oceanic system in Northeast Iran, has long been …
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 …
data to analyze the present‐day kinematics and the slip rates on most seismogenic faults in …
Tectonic setting and geochronology of the Cadomian (Ediacaran-Cambrian) magmatism in central Iran, Kuh-e-Sarhangi region (NW Lut Block)
The structure, age and petrogenesis of plutonic basement rocks from the Kuh-e-Sarhangi
region, located in the Kashmar-Kerman tectonic zone of Central Iran are described. These …
region, located in the Kashmar-Kerman tectonic zone of Central Iran are described. These …
Sabzevar Ophiolite, NE Iran: Progress from embryonic oceanic lithosphere into magmatic arc constrained by new isotopic and geochemical data
Abstract The poorly known Sabzevar–Torbat-e-Heydarieh ophiolite belt (STOB) covers a
large region in NE Iran, over 400 km EW and almost 200 km NS. The Sabzevar mantle …
large region in NE Iran, over 400 km EW and almost 200 km NS. The Sabzevar mantle …
The Arabia–Eurasia Collision Zone in Iran: Tectonostratigraphic and Structural Synthesis
The Arabia–Eurasia collision zone in the central part of the Alpine–Himalayan orogenic
system has had a complex deformation history since the Palaeozoic. In Iran, the collision …
system has had a complex deformation history since the Palaeozoic. In Iran, the collision …
Slab folding and surface deformation of the Iran mobile belt
A Boutoux, A Briaud, C Faccenna, P Ballato… - …, 2021 - Wiley Online Library
Back‐arc regions are usually punctuated by pulses of tectonic deformation, lasting for few
tens of millions of years. Yet, the origin of those short‐lived deformation episodes is …
tens of millions of years. Yet, the origin of those short‐lived deformation episodes is …
The post‐Eocene evolution of the Doruneh Fault region (central Iran): The intraplate response to the Reorganization of the Arabia‐Eurasia collision zone
The Cenozoic deformation history of Central Iran has been dominantly accommodated by
the activation of major intracontinental strike‐slip fault zones, developed in the hinterland …
the activation of major intracontinental strike‐slip fault zones, developed in the hinterland …
The Cimmerian accretionary wedge of Anarak, Central Iran
The occurrence in Iran of several ophiolite belts dating between Late Palaeozoic to Triassic
poses several questions on the possible existence of various sutures marking the closure of …
poses several questions on the possible existence of various sutures marking the closure of …
The long‐term evolution of the Doruneh Fault region (Central Iran): A key to understanding the spatio‐temporal tectonic evolution in the hinterland of the Zagros …
A better understanding of intraplate deformation requires the knowledge of the space–time
scales involved in its development and to decipher possible links with the dynamic evolution …
scales involved in its development and to decipher possible links with the dynamic evolution …
Neogene to Present paleostress field in Eastern Iran (Sistan belt) and implications for regional geodynamics
We conducted a stress field analysis of the northern part of the~ 700 km long north‐south
trending, seismically active Sistan orogenic belt of Eastern Iran formed as a result of the …
trending, seismically active Sistan orogenic belt of Eastern Iran formed as a result of the …