Formation of glacier runoff on the northern slope of Tavan Bogd mountain massif based on stable isotopes data

This investigation is based on measurements of stable isotopes concentrations (δD and δ18О) in water, snow and ice samples. Glaciers are composed of ice, snow, and fi n of atmospheric origin. The isotopic composition of these components is different, so when melting they form the melted glacial wate...

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Bibliographic Details
Main Authors: D. V. Bantsev, D. A. Ganyushkin, K. V. Chistyakov, A. A. Ekaykin, I. V. Tokarev, I. V. Volkov
Format: Article
Language:Russian
Published: Nauka 2018-09-01
Series:Lëd i Sneg
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/484