geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2014Research ArticleНаучные сообщенияShort communicationsО характере сопряжения морфоструктур ПрииссыккульяOn the morphostructures contacts character at the Issyk Kul regionШмидтГ. А.ShmidtG. A.ПНИИИС Госстроя СССРРоссия19792006202204Геоморфология8589Copyright © Шмидт Г.А., 20222022Шмидт Г.А.Shmidt G.A.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/2014

Morphostructures of the Issyk Kul region are characterised with asymmetry. One of morphostructures limbs is usually broken by neotectonic fault, Three types of morphostructures contacts are identified at the Issyk Kul region, i. e. stepped, adyr-stepped and contrasting ones. Zones of morphostructures can either gradually change one into another or have fault boundaries. The contact zones are 2 to 20 km width. Distribution of strong earthquakes epicenters reveals their connection with contrasting type of morphostructures contacts.

Morphostructures of the Issyk Kul region are characterised with asymmetry. One of morphostructures limbs is usually broken by neotectonic fault, Three types of morphostructures contacts are identified at the Issyk Kul region, i. e. stepped, adyr-stepped and contrasting ones. Zones of morphostructures can either gradually change one into another or have fault boundaries. The contact zones are 2 to 20 km width. Distribution of strong earthquakes epicenters reveals their connection with contrasting type of morphostructures contacts.

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