The data here provided have been used to analyse the structural evolution of the Arusan sector of the Great Kavir - Doruneh Fault system in Central Iran, one of the major intracontinental active strike-slip faults extending from the Afghan border to the Nain region between Central Iran and the Sanandaj-Sirjan Zone. We document important dextral shearing recorded along a segment of the GKDFS, the Arusan Fault System (AFS), located east of Jandaq, close to the present-day active trace of the GKDFS. The AFS include several ENE-WSW striking strands exposed for a length of more than 50 km, which couple pre-Cretaceous ophiolites and metamorphic basement units with the Cretaceous succession of the Khur basin. The fault shows transpressional struct...
The Alborz is a region of active deformation within the Arabia-Eurasia collision zone. The Abr and t...
This research assessed stress regimes and fields in eastern Iran using fault-slip data and the tecto...
The 856 A.D. Qumis earthquake (M7.9) is the most destructive earthquake to have occurred in Iran, ki...
The structural analysis of large intracontinental wrench faults is fundamental for deciphering the l...
Right-lateral shear between central Iran and Afghanistan is accommodated on N-S right-lateral strike...
Late Cenozoic strike-slip tectonics and active faulting in Central Iran have been extensively descri...
A better understanding of intraplate deformation requires the knowledge of the space–time scales inv...
The Cenozoic deformation history of Central Iran has been dominantly accommodated by the activation ...
International audienceThe NW trending Zagros fold-and-thrust belt is affected by two major dextral f...
A better understanding of intraplate deformation requires the knowledge of the space–time scales in...
times in response to Arabia-Eurasia convergence. The western Fars highlights a major bend of the def...
The NW–SE trending Sanandaj–Sirjan Zone (SSZ) is the internal part of the Zagros continental collisi...
International audienceThe Doruneh Fault System (DFS) is one of the major active strike-slip faults i...
International audienceThe Alborz is a region of active deformation within the Arabia-Eurasia collisi...
Late Cenozoic strike-slip tectonics and active faulting in Central Iran have been extensively descri...
The Alborz is a region of active deformation within the Arabia-Eurasia collision zone. The Abr and t...
This research assessed stress regimes and fields in eastern Iran using fault-slip data and the tecto...
The 856 A.D. Qumis earthquake (M7.9) is the most destructive earthquake to have occurred in Iran, ki...
The structural analysis of large intracontinental wrench faults is fundamental for deciphering the l...
Right-lateral shear between central Iran and Afghanistan is accommodated on N-S right-lateral strike...
Late Cenozoic strike-slip tectonics and active faulting in Central Iran have been extensively descri...
A better understanding of intraplate deformation requires the knowledge of the space–time scales inv...
The Cenozoic deformation history of Central Iran has been dominantly accommodated by the activation ...
International audienceThe NW trending Zagros fold-and-thrust belt is affected by two major dextral f...
A better understanding of intraplate deformation requires the knowledge of the space–time scales in...
times in response to Arabia-Eurasia convergence. The western Fars highlights a major bend of the def...
The NW–SE trending Sanandaj–Sirjan Zone (SSZ) is the internal part of the Zagros continental collisi...
International audienceThe Doruneh Fault System (DFS) is one of the major active strike-slip faults i...
International audienceThe Alborz is a region of active deformation within the Arabia-Eurasia collisi...
Late Cenozoic strike-slip tectonics and active faulting in Central Iran have been extensively descri...
The Alborz is a region of active deformation within the Arabia-Eurasia collision zone. The Abr and t...
This research assessed stress regimes and fields in eastern Iran using fault-slip data and the tecto...
The 856 A.D. Qumis earthquake (M7.9) is the most destructive earthquake to have occurred in Iran, ki...