gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2020-11-1-0461gtcrust-983Research ArticleСОВРЕМЕННАЯ ГЕОДИНАМИКАRECENT GEODYNAMICSСЕЙСМОТЕКТОНИКА ВНУТРЕННЕГО ТЯНЬ-ШАНЯ: СУУСАМЫРСКАЯ ВПАДИНА И ПРИЛЕГАЮЩИЕ ТЕРРИТОРИИSEISMOTECTONICS OF THE INNER TIENSHAN: SUUSAMYR BASIN AND ADJACENT AREAShttps://orcid.org/0000-0002-0247-1856МиколайчукА. В.MikolaichukA. V.

АЛЕКСАНДР ВЛАДИМИРОВИЧ МИКОЛАЙЧУК канд. геол.-мин. наук, с.н.с.

720481, г. Бишкек, бул. Эркиндик, 30, Кыргызстан

ALEXANDER V. MIKOLAICHUK Candidate of Geology and Mineralogy, Senior Researcher

30 Erkindyk Blvd, Bishkek 720481, Kyrgyzstan

alexander@mikolaichuk.comhttps://orcid.org/0000-0001-5172-3741КальметьеваЗ. А.KalmetyevaZ. A.

ЗОЯ АРСЛАНОВНА КАЛЬМЕТЬЕВА канд. физ.-мат. наук, с.н.с.

720027, г. Бишкек, ул. Тимура Фрунзе, 73/2, Кыргызстан

ZOYA A. KALMETEVA Candidate of Physical and Mathematical sciences, Senior Researcher

73/2 Timur Frunze Rd, Bishkek 720027, Kyrgyzstan

z.kalmetyeva@caiag.kghttps://orcid.org/0000-0002-4927-4729БургЖ.-П.BurgJ.-P.

ЖАН-ПЬЕР БУРГ докт., профессор геологии

СН-8092, г. Цюрих, Зоннегштрассе, 5, Швейцария

JEAN-PIERRE BURG Doctor, Full Professor of Geology

5 Sonneggstrasse, Zurich CH-8092, Switzerland

jean-pierre.burg@erdw.ethz.chhttps://orcid.org/0000-0003-3995-6336ФоссатиД.FossatiD.

ДЭВИД ФОССАТИ инженер

3302, г. Мосзеедорф, Зеедорфельдштрассе, 21, Швейцария

DAVID FOSSATI Geological Engineer

21 Seedorffeldstrasse, Moosseedorf 3302, Switzerland

dfoss81@hotmail.comhttps://orcid.org/0000-0001-8287-1018ГордеевД. В.GordeevD.V.

ДМИТРИЙ ВАЛЕНТИНОВИЧ ГОРДЕЕВ аспирант

720481, г. Бишкек, бул. Эркиндик, 30, Кыргызстан

DMITRY V. GORDEEV Post-graduate Student

30 Erkindyk Blvd, Bishkek 720481, Kyrgyzstan

d.gordeev56@outlook.comИнститут геологии НАНКыргызстанInstitute of Geology of NASKyrgyzstanЦентрально-Азиатский институт прикладных исследований ЗемлиКыргызстанCentral-Asian Institute for Applied GeosciencesKyrgyzstanДепартамент наук о Земле, Высшая техническая школаШвейцарияDepartment of Earth Sciences, ETHSwitzerlandДепартамент наук о Земле, Высшая техническая школа; Компания «Marti Tunnelbau AG»ШвейцарияDepartment of Earth Sciences, ETH; Marti Tunnelbau AGSwitzerland2020190320201113952Copyright © Миколайчук А.В., Кальметьева З.А., Бург Ж., Фоссати Д., Гордеев Д.В., 20202020Миколайчук А.В., Кальметьева З.А., Бург Ж., Фоссати Д., Гордеев Д.В.Mikolaichuk A.V., Kalmetyeva Z.A., Burg J., Fossati D., Gordeev D.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/983

Суусамырское землетрясение (М=7.3) произошло 19 августа 1992 г. в предположительно асей­смичном районе. Поскольку это событие оказалось неожиданным, оно привлекло внимание исследователей в области сейсмологии и сейсмотектоники всего мира. Однако результаты данных исследований не нашли отражения на последней карте сейсмического районирования Кыргызстана. Новые структурные исследования активных разломов и механизмов очагов землетрясений Суусамырской впадины и прилегающих территорий дают основание пересмотреть сложившиеся представления о сейсмичности региона. Сейсмическая опасность во Внутреннем Тянь-Шане (Ммах) представляется сопоставимой с таковыми в Северном и Южном Тянь-Шане, где были зарегистрированы многочисленные разрушительные события XIX и XX века. Полученные данные желательно учитывать на юге изученной территории, где планируется строительство гидроэлектростанций Нарынского каскада.

The Ms=7.3 Suusamyr earthquake of August 19, 1992 occurred in an area reputedly aseismic. Because it was not expected there, this event attracted worldwide attention of researchers in seismology and seismotectonics, but their results have not been included in the most recent seismic zoning map of Kyrgyzstan. New studies of neotectonic structures and focal mechanisms of earthquakes in the Suusamyr area and adjacent areas give reason to revise the established notions about the seismicity of the region. The seismic hazard in Inner Tienshan appears important and Mmax are comparable to those of the Northern and Southern Tienshan, where numerous destructive events were documented in the XIX and XX centuries. For the southern parts of the study area, along Naryn River, where hydroelectric power stations are planned, the new data should be used.

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The authors declare that there are no conflicts of interest present.