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палеоклимат
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CLIMATIC VARIABILITY IN THE ERA OF MIS‑11 (370–440 KA BP) ACCORDING TO ISOTOPE COMPOSITION (ΔD, Δ18O, Δ17O) OF ICE FROM THE VOSTOK STATION CORES
by
A. N. Veres
,
A. A. Ekaykin
,
D. O. Vladimirova
,
A. V. Kozachek
,
V. Ya. Lipenkov
,
A. A. Skakun
Published in
Ice and Snow
(2018)
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антарктида
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ледяной керн
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морская изотопная стадия 11
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палеоклимат
стабильные изотопы воды
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