Some Problems in Stratigraphic Analysis of Fir in Mizuho Plateau, East Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)

Long-term variation of precipitation and surface temperature in the vicinity of Mizuho Station were studied by means of stratigraphic analyses of 150-m boring core. ln this paper, some problems on snow stratigraphy aroused concerning the analyses are discussed. First, problems on the unit of stratif...

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Main Authors: Okitsugu WATANABE, Kikuo KATO, Kazuhide SATOW
Format: Article
Language:English
Published: National Institute of Polar Research 1979-10-01
Series:Antarctic Record
Online Access:https://doi.org/10.15094/00008093
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spelling doaj-6a624f387ece4f12b2d57d306852f22c2020-11-24T21:02:16ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X1979-10-0167325010.15094/00008093Some Problems in Stratigraphic Analysis of Fir in Mizuho Plateau, East Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology) Okitsugu WATANABE0Kikuo KATO1Kazuhide SATOW2Water Research Institute, Nagoya UniversityWater Research Institute, Nagoya UniversityNagaoka Technical CollegeLong-term variation of precipitation and surface temperature in the vicinity of Mizuho Station were studied by means of stratigraphic analyses of 150-m boring core. ln this paper, some problems on snow stratigraphy aroused concerning the analyses are discussed. First, problems on the unit of stratification are discussed in relation to visible stratigraphic elements and deposition-erosion processes Second, phenomena of missing layer corresponding to the hiatus in the layer formation are discussed in relation to regional characteristics of those occurrence and frequency. Precise estimation of mean annual accumulation in a certain perlod may be impossible without quantitative rating of hiatus duration, and establishment of an effective method of rating should be the most important subject for the stratigraphic study. δ^<18>O vertical profiles in snow layer are investigated using the data obtained from high-accumulation area (W46,1958 m a s.l,) in terms of reconsideration of the classical interpretation. As a result, it is found that a part of δ^<18>O oscillation was due to the variation by isotopic discrimination under snow metamorphism https://doi.org/10.15094/00008093
collection DOAJ
language English
format Article
sources DOAJ
author Okitsugu WATANABE
Kikuo KATO
Kazuhide SATOW
spellingShingle Okitsugu WATANABE
Kikuo KATO
Kazuhide SATOW
Some Problems in Stratigraphic Analysis of Fir in Mizuho Plateau, East Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)
Antarctic Record
author_facet Okitsugu WATANABE
Kikuo KATO
Kazuhide SATOW
author_sort Okitsugu WATANABE
title Some Problems in Stratigraphic Analysis of Fir in Mizuho Plateau, East Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)
title_short Some Problems in Stratigraphic Analysis of Fir in Mizuho Plateau, East Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)
title_full Some Problems in Stratigraphic Analysis of Fir in Mizuho Plateau, East Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)
title_fullStr Some Problems in Stratigraphic Analysis of Fir in Mizuho Plateau, East Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)
title_full_unstemmed Some Problems in Stratigraphic Analysis of Fir in Mizuho Plateau, East Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)
title_sort some problems in stratigraphic analysis of fir in mizuho plateau, east antarctica (special issue of the proceedings of the first symposium on antarctic meteorology and glaciology)
publisher National Institute of Polar Research
series Antarctic Record
issn 0085-7289
2432-079X
publishDate 1979-10-01
description Long-term variation of precipitation and surface temperature in the vicinity of Mizuho Station were studied by means of stratigraphic analyses of 150-m boring core. ln this paper, some problems on snow stratigraphy aroused concerning the analyses are discussed. First, problems on the unit of stratification are discussed in relation to visible stratigraphic elements and deposition-erosion processes Second, phenomena of missing layer corresponding to the hiatus in the layer formation are discussed in relation to regional characteristics of those occurrence and frequency. Precise estimation of mean annual accumulation in a certain perlod may be impossible without quantitative rating of hiatus duration, and establishment of an effective method of rating should be the most important subject for the stratigraphic study. δ^<18>O vertical profiles in snow layer are investigated using the data obtained from high-accumulation area (W46,1958 m a s.l,) in terms of reconsideration of the classical interpretation. As a result, it is found that a part of δ^<18>O oscillation was due to the variation by isotopic discrimination under snow metamorphism
url https://doi.org/10.15094/00008093
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