THE LOSS FROM THE UPPER LAYER OF BOTTOM SEDIMENTS IN THE CORES FROM BOREHOLES BDP-96-1 AND BDP-96-2 (DRILLED ON LAKE BAIKAL)

dc.contributor.author	Karabanov E.B.
dc.contributor.author	Kuz'min M.I.
dc.contributor.author	Geletii V.F.
dc.contributor.author	Kalraychkov G.V.
dc.contributor.author	Gvozdkov A.N.
dc.date.accessioned	2021-01-13T07:39:07Z
dc.date.available	2021-01-13T07:39:07Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=14997019
dc.identifier.citation	Geologiya i geofizika, 1999, , 8, 1269-1271
dc.identifier.issn	0016-7886
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22880
dc.description.abstract	In 1996, boreholes BDP-96-1 and BDP-96 penetrated the bottom sediments of Lake Baikal. From the lithological and geochemical correlation of the sediments, the loss from the upper layer of sediments in the cores is estimated: 630 cm (BDP-96-1) and 19 cm (BDP-96-2). Correlation of these cores with the 120 cm long core from borehole GC-1, taken with a gravity corer during the drilling through the lake ice, permits compilation of a general continuous record of climatic changes in Central Asia for the last 5 Ma and prevention of loss of Holocene sediments.
dc.subject	Holocene	en
dc.title	THE LOSS FROM THE UPPER LAYER OF BOTTOM SEDIMENTS IN THE CORES FROM BOREHOLES BDP-96-1 AND BDP-96-2 (DRILLED ON LAKE BAIKAL)
dc.type	Статья
dc.subject.age	Cenozoic::Quaternary::Holocene	en
dc.subject.age	Кайнозой::Четвертичная::Голоцен	ru

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