Sapropelic, diatomaceous and coccolith sediments (units Ib, Ia) of The Black sea bottom – genesis, composition and properties

Holocene Black Sea basin sediments were formed in our opinion in happened geocatastrofic event on the border Pleistocene–Holocene (8–9 thousand years ago). As a result on the Upper Pleistocene lake sediments occur organogenic mineral (sapropel diatoms and coccolith) marine sediments. The charact...

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Published in:Геология и полезные ископаемые Мирового океана
Date:2011
Main Author: Dimitrov, D.
Format: Article
Language:English
Published: Відділення морської геології та осадочного рудоутворення НАН України 2011
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Online Access:https://nasplib.isofts.kiev.ua/handle/123456789/44536
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Journal Title:Digital Library of Periodicals of National Academy of Sciences of Ukraine
Cite this:Sapropelic, diatomaceous and coccolith sediments (units Ib, Ia) of The Black sea bottom – genesis, composition and properties / D. Dimitrov // Геология и полезные ископаемые Мирового океана. — 2011. — № 1. — С. 5-19. — Бібліогр.: 35 назв. — англ.

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Digital Library of Periodicals of National Academy of Sciences of Ukraine