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 |
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| Date: | 2011 |
| Main Author: | |
| Format: | Article |
| Language: | English |
| Published: |
Відділення морської геології та осадочного рудоутворення НАН України
2011
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| Subjects: | |
| 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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