Hissar–Alai and the Pamirs: Junction and Position in the System of Mobile Belts of Central Asia

The position of the Pamirs and the Hissar–Alai mountainous system in the structure of Central Asia and features of their junction are considered. It is shown that their outer contours and tectonic infrastructure are significantly distinct in the planar pattern: latitudinally linear and arched for the Hissar–Alai and the Pamirs, respectively. These structures logically match those of the Central Asian and Alpine–Himalayan belts, respectively. The Pamir orogen is a relatively autonomous structural element of the crust, which is located discordantly relative to the country lithospheric blocks. Most of the Pamirs (at least, the Northern and Central) probably form a giant allochthon on the ancient basement of the Tarim and Afghan–Tajik blocks. The junction zone of these two “hard” crustal segments is reflected in the transverse Transpamir threshold, which is expressed in the relief, deep structure, and seismicity. The specific geological structure of the junction zone of the Pamirs and Hissar–Alai (systems of the Tarim, Alai, and Afghan–Tajik troughs) is shown. It suggested that this zone is a damper, which significantly neutralizes the dynamic influence of the Pamir and the southernmost elements of the Pamir–Punjab syntax on Hissar–Alai structures.