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The deposits sourrounding late Pleistocene massive ice bodies in the region o...
This dataset has no description
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δ²H in ice wedge, sand wedge, massive and pore ice at Rogozhny Cape, northern...
δ²H in ice wedge (IW), sand wedge (SIW), massive (MI) and pore (PI) ice at Rogozhny Cape, northern coast of Onemen Gulf, 25 km from Anadyr Town. -
δ¹⁸O in ice wedge and pore ice from vicinity of Anadyr Town
Major ions and dissolved salts in syngenetic ice wedges in the 25–30 m thick Late Pleistocene Ledovy Obryv yedoma and the 60-m thick Ust'-Algan Obryv yedoma. -
δ¹⁸O variations in ice wedge and pore ice from Ledovy Obryv and Ust'-Algan ou...
This dataset has no description
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Major ion chemistry of Late Pleistocene permafrost from outcrop samples of th...
This dataset has no description
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δ¹⁸O variations in Late Pleistocene and Holocene ice wedges and in growing pr...
This dataset has no description
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Stable isotope (δ18О, δ2H and dexc) minimum, mean, and maximum values for mas...
Stable oxygen and hydrogen compositions in ice were analyzed in the stable isotope laboratory of the Faculty of Geography at Lomonosov Moscow State University using a Finnigan... -
AMS radiocarbon ages of three massive ice bodies on the coast of Mechigmen Ba...
Radiocarbon dating of micro-inclusions of organic material extracted directly from massive ice samples was carried out at the Laboratory of Radiocarbon Dating and Electron... -
Water-soluble salts in the syngenetic ice wedges of Late-Pleistocene yedoma a...
Composition and content of water-soluble salts in the syngenetic ice wedges of the 25–30-m Late-Pleistocene yedoma and in the modern ices and the water reservoirs of Ayon... -
Water-soluble salts in the syngenetic permafrost deposits of Late- Pleistocen...
The composition and content of water-soluble salts in the syngenetic permafrost deposits of the 25–30-m Late- Pleistocene yedoma of Ayon Island. -
δ¹⁸O in the Late-Pleistocene and Holocene ice wedges and segregated schlieren...
Variations in δ18О values in the Late-Pleistocene (pIW) and Holocene (hIW) ice wedges and segregated ice schlieres (SIS) ices of Ayon Island.# = Isotopic analyses were... -
δ¹⁸O in ice wedges, ice lenses and snow from Kular, Yakutia (Russia)
Variations of δ¹⁸О in Late Pleistocene ice wedges, in structure-forming ice and segregated ice lenses, as well as in snow and water of Burguat River were determined. The studied... -
Trace elements and alkaline-earth metals in Late Pleistocene syngenetic ice w...
Content of trace elements and alkaline-earth metals in Late Pleistocene syngenetic ice wedges from Kular in Northern Yakutia. Analytical measurements of the trace element... -
Composition and content of water-soluble salts in syngenetic ice wedges in Ku...
Composition and content of water-soluble salts in syngenetic ice wedges from Kular in Northern Yakutia. The chemical composition of water-soluble salts in the Late Pleistocene... -
Composition and content of water-soluble salts (%) in yedoma Late Pleistocene...
Composition and content of water-soluble salts in yedoma Late Pleistocene deposits from Kular in Northern Yakutia. The chemical composition of water-soluble salts in the Late... -
Content of water-soluble salts in sediments from the outcrop of the Ery-Maret...
Data was compiled from G.E. Oblogov, 2016. -
Content and composition of water-soluble salts in the sediments of the second...
Content and composition of water-soluble salts in the sediments of the second lagoon-marine terrace, in the lower reaches of the Mongatalyangyakha River on the Yavai Peninsula... -
δ¹⁸O, δ²H and dexc values in ice wedges and segregated ice interlayer from th...
Data was compiled from G.E. Oblogov, 2016. -
Dole effect in the north of the South China Sea from sediment core PC27 and PC83
Relative intensity proxy (RPI) be constructed using the equation: RPI=NRM/SIRM (20-60)mT * MDFSIRM-CM/MDFSIRM, where MDFSIRM-CM is the center of mass of MDFSIRM.Dole effect was... -
Inclination of the South China Sea from sediment core PC27, PC83 and PC111
Normal remanent magnetization (NRM) and stepwise alternating field (AF) demagnetization were performed on the box samples with peak fields of 0-90 mT in 10-mT step and analysed...
