δ18O and δD variations in Holocene massive ice in the Sabettayakha river mouth, northern Yamal Peninsula

被引：0
|
作者：
Yu. K. Vasil’chuk
Ye. Ye. Podborny
N. A. Budantseva
A. C. Vasil’chuk
A. N. Sullina
Ju. N. Chizhova
机构：
[1] Moscow State University,
[2] ООО Center for Hydroecological Studies,undefined
来源：
Doklady Earth Sciences | 2016年 / 470卷
关键词：
D O I：
暂无
中图分类号：
学科分类号：
摘要：
The conditions of formation of massive ice near the South Tambey gas-condensate field in northern Yamal Peninsula are studied. It is shown that massive ice bodies up to 4.5 m thick occur in the Holocene deposits of the high laida and the first terrace. Therefore, they cannot be the remains of glaciers; they are ground ice formations. All three types of massive ice have quite various isotopic compositions: the values of δD range from–107 to–199.7, and δ18O from–15.7 to–26.48‰. Such a significant differentiation in isotopic composition is a result of cryogenic fractionation in a freezing water-saturated sediment. The most negative isotope values are even lower in this Holocene massive ice than in the Late Pleistocene ice-wedge ice of Yamal Peninsula.
引用
收藏
页码：1086 / 1092
页数：6
相关论文
共 50 条
  • [31] Spatial variations of δD and δ18O in lake water of western China and their controlling factors
    Feng S.
    Liu X.
    Li H.
    Liu, Xingqi (xqliu@cnu.edu.cn), 1600, Science Press (32): : 1199 - 1211
  • [32] Origins of the Rio Capim kaolinites (northern Brazil) revealed by δ18O and δD analyses
    dos Santos, Antonio Emidio de Araujo, Jr.
    Rossetti, Dilce de Fatima
    Murray, Haydn H.
    APPLIED CLAY SCIENCE, 2007, 37 (3-4) : 281 - 294
  • [33] Temporal and Spatial Variations of Precipitation δ18O and Controlling Factors on the Pearl River Basin and Adjacent Regions
    Ruan, Yunfeng
    Liu, Zhaofei
    Yao, Zhijun
    Wang, Rui
    ADVANCES IN METEOROLOGY, 2018, 2018
  • [34] δ18O and δD records of inactive ice wedge in Yitulihe, Northeastern China and their paleoclimatic implications
    SiZhong Yang
    HuiJun Jin
    Science China Earth Sciences, 2011, 54 : 119 - 126
  • [35] δ18O and δD records of inactive ice wedge in Yitulihe, Northeastern China and their paleoclimatic implications
    Yang SiZhong
    Jin HuiJun
    SCIENCE CHINA-EARTH SCIENCES, 2011, 54 (01) : 119 - 126
  • [36] δ18O and δD records of inactive ice wedge in Yitulihe, Northeastern China and their paleoclimatic implications
    YANG SiZhong & JIN HuiJun State Key Laboratory of Frozen Soils Engineering
    ScienceChina(EarthSciences), 2011, 54 (01) : 119 - 126
  • [37] Holocene climate variability in Europe:: Evidence from δ18O, textural and extension-rate variations in three speleothems
    McDermott, F
    Frisia, S
    Huang, YM
    Longinelli, A
    Spiro, B
    Heaton, THE
    Hawkesworth, CJ
    Borsato, A
    Keppens, E
    Fairchild, IJ
    van der Borg, K
    Verheyden, S
    Selmo, E
    QUATERNARY SCIENCE REVIEWS, 1999, 18 (8-9) : 1021 - 1038
  • [38] Water and carbon cycles in the Han River Basin, Korea constrained from δD and δ18O of the river water
    Lee, D
    Lee, KS
    Woo, NC
    Kim, Y
    GEOCHIMICA ET COSMOCHIMICA ACTA, 2003, 67 (18) : A247 - A247
  • [39] Changes of δ18O and δD along the Dousitu River, Inner Mongolia, China, and their evidence of river water evaporation
    Qian Hui
    Li Mengyao
    Ji Yadong
    Yang Bingchao
    Zhao Zhenhong
    Aquatic Geochemistry, 2007, 13 : 127 - 142
  • [40] Changes of δ18O and δD along the Dousitu River, Inner Mongolia, China, and their evidence of river water evaporation
    Hui, Qian
    Li, Mengyao
    Ji, Yadong
    Yang, Bingchao
    Zhao, Zhenhong
    AQUATIC GEOCHEMISTRY, 2007, 13 (02) : 127 - 142
12345