FACIAL PALEOGEOGRAPHIC CONDITIONS FOR THE FORMATION OF PALEOCENE-LOWER EOCENE DEPOSITS OF FERGANA DEPRESSION

Authors

  • Pulatjon Sultonov , Bakhodir Meliboyev , Farkhod Chulliev, Mansur Ruziev

Abstract

As result of facial-paleogeographic studies of the Paleogene deposits of the Fergana
depression are distinguished underwater delta, wave-cut, shallow-bay (lagoon) and centraldesilting facial belts. The article gives a detailed description of the lagoon facies with their
separation into 4 types, which can be the criteria for the prospecting and exploration of
nonmetallic minerals, such as palygorskite clays, dolomites and gypsum.

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Published

2020-12-01

How to Cite

Pulatjon Sultonov , Bakhodir Meliboyev , Farkhod Chulliev, Mansur Ruziev. (2020). FACIAL PALEOGEOGRAPHIC CONDITIONS FOR THE FORMATION OF PALEOCENE-LOWER EOCENE DEPOSITS OF FERGANA DEPRESSION. PalArch’s Journal of Archaeology of Egypt / Egyptology, 17(6), 3642 - 3657. Retrieved from http://mail.palarch.nl/index.php/jae/article/view/1480