Mineral Composition, Structure and Texture of the Paleogene Period Carbonate Deposits in the Aksokota River Basin

Authors

  • Khamrakulov Mansurzhon Abdukholikovich senior lecturer Namangan Engineering and Construction Institute.
  • Kurbanbayev Aslbek Otabekov Namangan Engineering and Construction Institute student.
  • Mukimov Azizbek Ibrohimjon ugli Namangan Engineering and Construction Institute student.
  • Dadamirzayev Samandar Zoyirjon ugli Namangan Engineering and Construction Institute student.

Abstract

Studying the structure and texture of Aksokota opens a wide way to search for new oil
and gas deposits in the current period. The oil and gas industry is developing rapidly. The main
future task of geologists working in the oil and gas sector is to contribute to the national economy.
It is an independent branch of geotectonics, which studies the structure of the earth's crust and the
laws of its development.

References

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clay minerals and their application in deep well drilling in difficult conditions of

Uzbekistan. Tashkent, Science, 1978. 80 s.

Zokirov M. Z. Hypergenesis of clay deposits of Uzbekistan and its mineral indicators.

Tashkent, science, 1977, 182 p.

Mirzayev A. U., Chinikulov X. New deposit of Nabalor bentonite clays. Geology and

mineral resources.1999. Nº5, C.23-30.

Mirzayev A. U. Chinikulov X., Tsoi L. A. Carbonate clays of the Navbahor deposit UzR.

, No. 5, Page 30.

Ibragimov R.N. Methods of deep geological mapping ipoiskov poleznyx iskopaemyx.

Tashkent, NUUz, 2004.

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Published

2024-10-31

How to Cite

Khamrakulov Mansurzhon Abdukholikovich, Kurbanbayev Aslbek Otabekov, Mukimov Azizbek Ibrohimjon ugli, & Dadamirzayev Samandar Zoyirjon ugli. (2024). Mineral Composition, Structure and Texture of the Paleogene Period Carbonate Deposits in the Aksokota River Basin . American Journal of Open University Education, 1(8), 170–173. Retrieved from https://scientificbulletin.com/index.php/AJOUP/article/view/325