Use of stable water isotopes to identify stages of the pingo ice core formation

Te isotopic characteristics of the pingo ice cores are considered. Te distribution of δ18O and δ2H values, dexc, δ18O–δ2H and δ2H–d exc relationships, and the simulation of the distribution of δ18O and δ2H values during the ice formation in a closed system, allowed drawing conclusion about the hydro...

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Bibliographic Details
Main Authors: Ju. N. Chizhova, Yu. K. Vasil’chuk
Format: Article
Language:Russian
Published: Nauka 2018-12-01
Series:Лëд и снег
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/513