LATE MIOCENE VOLCANIC ASH LAYERS OF THE INTERMOUNTAIN DEPRESSION OF THE EASTERN CAUCASUS: THE PRODUCTS OF THE MEGACALDERA EXPLOSION?

Okrostsvaridze, Avtandil და Gagnidze, Nona და Bobrova, Iulia და Skhirtladze, Irakli (2017) LATE MIOCENE VOLCANIC ASH LAYERS OF THE INTERMOUNTAIN DEPRESSION OF THE EASTERN CAUCASUS: THE PRODUCTS OF THE MEGACALDERA EXPLOSION? Proceedings of Joint meeting of IGCP 610 project.

ტექსტი Proc. IGCP_Pr 610.A.O. Vol.Ash-2017.pdf Download (2MB)

რეზიუმე

The Caucasus is a central segment of the Mediterranean Alpine-Himalayan collisional orogenic system and consists of the Greater and Lesser Caucasus orogens and intermountain depression. There are numerous layers of volcanic ashes in the late Miocene marine sediments (dated paleontologically) of the Eastern Caucasus intermountain depression. The ashes consist primarily of hornblende, pyroxene, and volcanic glass (Skhirtladze, 1964). The thickness of the layers varies between 5 m to several decimeters, while their distribution area is wide and includes the Kartli and Kakheti regions in Georgia and the western region of Azerbaijan

ობიექტის ტიპი:	სტატია
თემატიკა:	Q Science Q Science > QE Geology
განმათავსებელი მომხმარებელი:	ავთანდილ ოქროსცვარიძე
განთავსების თარიღი:	28 თებერვალი 2022 10:49
ბოლო ცვლილება:	28 თებერვალი 2022 10:49
URI:	http://eprints.iliauni.edu.ge/id/eprint/10994

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