SOME PECULIARITIES OF GEOLOGICAL STRUCTURE BETWEEN KOTUC AND VEDI RIVERS
(Yerevan-Vedi graben-synclinorium)
DOI:
https://doi.org/10.46991/PYSU:C/2007.41.1.111Keywords:
Kotuc River, Vedi River, olistostrom horizons, Yerevan-Vedi graben-synclinorium, modern geodynamics, geodynamic active structuresAbstract
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
How to Cite
Avanesyan, M. A. (2007). SOME PECULIARITIES OF GEOLOGICAL STRUCTURE BETWEEN KOTUC AND VEDI RIVERS: (Yerevan-Vedi graben-synclinorium). 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
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Geology
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Copyright (c) 2007 Proceedings of the YSU
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