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- > Special Issue : Stable isotopes and geochemistry of ground ice (supprimer)
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Par Collection Par Auteur- MEYER, H. (2)
- SLETTEN, R.S. (2)
- DEREVIAGIN, A.Y. (1)
- KIZYAKOV, A.I. (1)
- LEIN, A.Y. (1)
- MEYER, H. (1)
- PEREDNYA, D.D. (1)
- SAVVICHEV, A.S. (1)
- SCHIRRMEISTER, L. (1)
- VANSHTEIN, B.G. (1)
- WETTERICH, S. (1)
- LEIBMAN, M.O. (1)
- OPEL, T. (1)
- 2011 (2)
- Analyse isotopique ; Arctique ; Coin de glace ; Deutérium ; Géochimie ; Holocène ; Oxygène 18 ; Paléo-environnement ; Paléoclimat ; Pergélisol ; Russie d'Asie ; Sibir' (1)
- Analyse isotopique ; Arctique ; Glace ; Glace du sol ; Géochimie ; Humidité ; Littoral ; Périglaciaire ; Russie (1)
- Análisis isotópico ; Cuña de hielo ; Deuterio ; Geoquímica ; Holoceno ; Oxígeno 18 ; Paleoambiente ; Paleoclima ; Pergelisol ; Rusia de Asia ; Siberia ; Ártica (1)
- Análisis isotópico ; Geoquímica ; Hielo ; Hielo del suelo ; Humedad ; Litoral ; Periglaciar ; Rusia ; Ártica (1)
- Arctic Region ; Asian part of Russia ; Deuterium ; Geochemistry ; Holocene ; Ice wedge ; Isotope analysis ; Oxygen 18 ; Palaeo-environment ; Palaeoclimate ; Permafrost ; Siberia (1)
- Arctic Region ; Coastal environment ; Geochemistry ; Ground ice ; Ice ; Isotope analysis ; Moisture ; Periglacial features ; Russia (1)
- Special Issue : Stable isotopes and geochemistry of ground ice (2)
- Palaeoclimatic information from stable water isotopes of Holocene ice wedges on the Dmitrii Laptev Strait, northeast Siberia, Russia (1)
- Sulfur and carbon isotopes within atmospheric, surface and ground water, snow and ice as indicators of the origin of tabular ground ice in the Russian Arctic (1)
- The stable isotopic composition (andO 18, andD, d) of 3 Holocene-age ice wedges at the Dmitrii Laptev Strait was studied at high resolution in order to develop palaeoclimatic records. AMS C 14 ages of organic matter in the ice prove the Late
- Field sampling of tabular ground ice (TGI) was undertaken at a number of geological sections along the Russian Arctic coast. S 34 in sulfate ion and C 13 in organic matter were analysed in ground ice and enclosing deposits, and in reference samples