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...
Збережено в:
| Дата: | 2011 |
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| Автор: | |
| Формат: | Стаття |
| Мова: | English |
| Опубліковано: |
Відділення морської геології та осадочного рудоутворення НАН України
2011
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| Назва видання: | Геология и полезные ископаемые Мирового океана |
| Теми: | |
| Онлайн доступ: | http://dspace.nbuv.gov.ua/handle/123456789/44536 |
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| Назва журналу: | Digital Library of Periodicals of National Academy of Sciences of Ukraine |
| Цитувати: | 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. |
Репозитарії
Digital Library of Periodicals of National Academy of Sciences of Ukraine| Резюме: | 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 characteristic
features of happened catastrophe is the occurrence of hydrogen sulfide charging
that conserved the organic matter and protect it from decomposition. Chemical
composition and properties of deep water organogenic mineral deposits give us
reason to Tip of the raw material as an integrated multi purpose and most notably
in agriculture. |
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