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...
Published in: | Ice and Snow |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | Russian |
Published: |
Nauka
2018
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Subjects: | |
Online Access: | https://doi.org/10.15356/2076-6734-2018-4-507-523 https://doaj.org/article/f6e3793bf54b427cb49c7d9c3c5cbdac |