SEISMICALLY ACTIVE FAULTS OF SOUTHERN UZBEKISTAN

https://doi.org/10.69617/nuuz.v3i3.2.1.5763
Seismogenic, regional Faults, Structures, morphostructure, seismic, macroseismic, instrumental, stress, earthquake, assessment, vibration, ball, intensive, zone, isoseist, observatory, geophysical, rupture, geodynamic, geosynclinal, Southern Uzbekistan.

Authors

  • Bobur ZIYOMOV O‘zbekiston Milliy universiteti Geodinamika va tektonika dotsenti v.b., PhD , Uzbekistan
Vol. 3 No. 3.2.1 (2024): O'zMU XABARLARI (3.2.1 SONI) 2024 TABIIY FANLAR
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The article discusses the possibilities of studying the seismogenic zones of Southern Uzbekistan. Analysis of materials and identification of the main seismogenic zones at the regional level has established that they arise as a result of deformations associated, for example, with the movement of regional faults, structures, and tectonic blocks. It is known that the seismic process consists of the process of continuous accumulation of stresses in the earth's crust and their sudden disappearance.