About the Geological Structure of the Agstafachay-Ganjachay Valley Plain

Authors

  • S.I. Ibrahimova Azerbaijan State Oil and Industry University (Azadlıg ave. 20, Baku, AZ1010, Azerbaijan)
  • G.K. Aghamaliyeva Azerbaijan State Oil and Industry University (Azadlıg ave. 20, Baku, AZ1010, Azerbaijan)
  • A.Z. Nasibov Azerbaijan State Oil and Industry University (Azadlıg ave. 20, Baku, AZ1010, Azerbaijan)

DOI:

https://doi.org/10.52171/2076-0515_2024_16_04_120_126

Keywords:

bearing cone, lithological composition, sediments, sloping plain

Abstract

Jurassic, Cretaceous, Paleogene, Neogene and Quaternary sediments are involved in the geological structure of the Agstafachay-Ganjachay valley plain. Mesozoic sediments form the mountain outcrops of the Lesser Caucasus and reach the earth's surface along the mountain front. In the remaining areas, it is quite deep. Paleogene and Neogene sediments come to the surface in the southeast of the massif. All these sediments are covered by younger sediments in the foothill plain area.

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Published

2024-12-30

How to Cite

Ibrahimova, S., Aghamaliyeva, G., & Nasibov, A. (2024). About the Geological Structure of the Agstafachay-Ganjachay Valley Plain . Herald of Azerbaijan Engineering Academy, 16(4), 120–126. https://doi.org/10.52171/2076-0515_2024_16_04_120_126

Issue

Vol. 16 No. 4 (2024)

Section

Articles

License

Creative Commons License

This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.