ESR AND TL DATING OF QUATERNARY SEDIMENTS IN THE LUTZOW-HOLM BAY REGION, EAST ANTARCTICA

Fossil shells and marine sediments in the Lutzow-Holm Bay region, East Antarctica, were dated by electron spin resonance (ESR) and thermoluminescence (TL), respectively. The ESR and TL dates obtained in this study could be correlated with the postglacial ^<14>C age group around Lutzow-Holm Bay...

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Bibliographic Details
Main Authors: タカダ マサシ, ハヤシ マサヒサ, サワガキ タカノブ, ヒラカワ カズオミ, モリワキ キイチ, Masashi TAKADA, Masahisa HAYASHI, Takanobu SAWAGAKI, Kazuomi HIRAKAWA, Kiichi MORIWAKI
Format: Report
Language:English
Published: The University Museum, the University of Tokyo:(Present address)Faculty of Letters, Nara Women's University 1995
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2800
http://id.nii.ac.jp/1291/00002800/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2800&item_no=1&attribute_id=18&file_no=1
Description
Summary:Fossil shells and marine sediments in the Lutzow-Holm Bay region, East Antarctica, were dated by electron spin resonance (ESR) and thermoluminescence (TL), respectively. The ESR and TL dates obtained in this study could be correlated with the postglacial ^<14>C age group around Lutzow-Holm Bay. The sample of shells was taken from the emerged marine sediments in Langhovde which also contain another sample of quartz, and there is a small discrepancy between the two dates. Probably it is due to uncertainties in the estimates of the internal dose for the fossil shells and of the paleodose for the quartz sample.