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)
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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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