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MAGNETOSTRATIGRAPHY OF QUATERNARY DEPOSITS OF THE FERGANA DEPRESSION

Fergana depression, Quaternary deposits, paleomagnetic method, stratigraphy, eopleistocene, pleistocene, holocene, magnetic polarity, tectonic processes, geological sections

Authors

  • Ходжиакбар ТОЙЧИЕВ Д.г.-м.н., профессор Национального университета Узбекистана, Uzbekistan
  • Анна СТЕЛЬМАХ К.г.-м.н., доцент Национального университета Узбекистана, Uzbekistan
  • Нодира ТАДЖИБАЕВА, К.г.-м.н., доцент, заведующая кафедрой Геофизики и гидрогеологии Национального университета Узбекистана, Uzbekistan

The article presents the results of paleomagnetic studies of Quaternary deposits of the Fergana depression. In the process of study, a detailed description of the lithology, age and genesis of the deposits was carried out using paleomagnetic data, which made it possible to accurately determine the age and polarity of the geomagnetic field for various stratigraphic units. Based on paleomagnetic studies, the age boundaries of the eopleistocene, pleistocene and holocene deposits were determined, which made it possible to clarify the stratigraphic scheme of the region

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