SOME PECULIARITIES OF GEOLOGICAL STRUCTURE BETWEEN KOTUC AND VEDI RIVERS

(Yerevan-Vedi graben-synclinorium)

Authors

  • M. A. Avanesyan Chair of Historical and Regional Geology, YSU, Armenia

DOI:

https://doi.org/10.46991/PYSU:C/2007.41.1.111

Keywords:

Kotuc River, Vedi River, olistostrom horizons, Yerevan-Vedi graben-synclinorium, modern geodynamics, geodynamic active structures

Abstract

In this work are presented some new data about the geological structure of central part of one of the interesting and difficult structured tectonic units of Armenia – Yerevan-Vedi graben-synclinorium. For the first time are allocated and described the olistostrom horizons in the development field of paleocene sediments. Young ruptures are described, probably of seismogenic nature. Connection of modern geodynamics with geodynamic active structures of the geological past is considered.

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Published

2007-03-05

Issue

Vol. 41 No. 1 (212) (2007)

Section

Geology

License

Copyright (c) 2007 Proceedings of the YSU

Creative Commons License

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

How to Cite

SOME PECULIARITIES OF GEOLOGICAL STRUCTURE BETWEEN KOTUC AND VEDI RIVERS: (Yerevan-Vedi graben-synclinorium). (2007). Proceedings of the YSU C: Geological and Geographical Sciences, 41(1 (212), 111-116. https://doi.org/10.46991/PYSU:C/2007.41.1.111