In this contribution, we investigate the space and time distribution of the Cenozoic
magmatism and the associated porphyry Cu-Mo±Au and other hydrothermal (mostly …

Abstract The Eastern Iranian range is seen as a large scale India-Eurasia collisional event
and the subsequent amalgamation of the Afghan and Lut micro-continents, including the …

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 oblique collision between the northeastern margin of the Arabian platform and the
Iranian microcontinent has led to transpressional deformation in the Zagros orogenic belt in …

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 …

The pre-Alpine evolution of the Tethyan domains between Gondwana and Laurasia, and in
particular that of the Cimmerian continental blocks, remains poorly constrained. Central Iran …

We present two robust and well‐dated paleomagnetic poles from upper Eocene and
Oligocene volcanics in the Urumieh‐Dokhtar magmatic arc, Central Iran. These two poles …

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 …

Geodetic and seismological data are crucial for examining the kinematics and active
tectonics in structural zones. The current tectonic stress field can be inferred from the focal …

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 …