Seismic Catastrophes in Akhsiket (Akhsi), the Capital of Fergana, in the Epoch of Timur and the Timurids
А. М. КорженковSchmidt Institute of Physics of the Earth, Russian Academy of Sciences, 123995, Moscow, RussiaA. A. AnarbaevNational Center of Archaeology, Academy of Sciences, Republic of Uzbekistan, Tashkent, UzbekistanM. T. UsmanovaMavlyanov Institute of Seismology, Academy of Sciences, Republic of Uzbekistan, Tashkent, UzbekistanU. A. NurmatovMavlyanov Institute of Seismology, Academy of Sciences, Republic of Uzbekistan, Tashkent, UzbekistanSh. NasriddinovNamangan State University, Republic of Uzbekistan, Namangan, UzbekistanU. L. ArtikovNational Center of Archaeology, Academy of Sciences, Republic of Uzbekistan, Tashkent, UzbekistanT. K. ZakhidovMavlyanov Institute of Seismology, Academy of Sciences, Republic of Uzbekistan, Tashkent, UzbekistanU. A. YusupdzhanovaMavlyanov Institute of Seismology, Academy of Sciences, Republic of Uzbekistan, Tashkent, UzbekistanL. A. KorzhenkovaSergeev Institute of Geoecology, Russian Academy of Sciences, Moscow, RussiaA. A. SentsovSchmidt Institute of Physics of the Earth, Russian Academy of Sciences, 123995, Moscow, RussiaА. О. АгибаловSchmidt Institute of Physics of the Earth, Russian Academy of Sciences, 123995, Moscow, Russia
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Аннотация
Seismic deformations in the ruins of the ancient town of Yangi Akhsi (Namangan oblast, Uzbekistan) have been studied: ruptures with displacement in the ground, collapses over considerable distances, tilts, shifts, and rotations of the parts of buildings, formed as a result of at least two late medieval earthquakes. They are associated with the activation of the North Ferghana flexure-rupture zone. Based on the assessment of the period of recurrence of earthquakes in this area, it is concluded that conditions have currently formed here for the occurrence of a seismic event with a magnitude of 6 or higher.
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