Аннотация:The article presents a brief overview of the currently existing ideas about the seismotectonic situation in the Earth’s crust of Iran, which is experiencing intense compression in the northeastern direction as aresult of collision of the Arabian and Eurasian lithospheric plates. The survey also involved geodetic data inthe form of modern GPS measurements of horizontal surface displacements. The stress-strain state of theEarth’s crust of Iran (construction of the average focal mechanism) was assessed based on data on the totalset of 945 focal mechanisms of earthquakes of average strength (4.4 ≤ MW ≤ 6.5) according to the ISC catalog,which occurred from 1975 to 2020, within 12 spatial samplings. The focal mechanisms of the strongest earthquakes in the last 50 years (MW = 6.0–7.4) for one event in each of these samplings are also considered. Thecalculated parameters of the average mechanisms and focal mechanisms of strong earthquakes are comparedboth with each other and with the surrounding tectonic situation and the distribution of deformation velocityvectors according to GPS observations. A satisfactory correspondence has been established between all thecomparable values. The differences in the type of formation of the seismogenic layer of the Earth’s crust ofIran in different regions are demonstrated. These differences are manifested in different ratios of shear andthrust components in the reconstructed mean mechanism in different spatial samplings. A similar differenceis noted in individual focal mechanisms of the strongest earthquakes. However, it is possible to describe theobserved nature of deformation of the crust of Iran within a single concept of collisional tectonics, caused bycollision of the Arabian and Eurasian plates in the last 5 Ma