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最終氷期最盛期以降の南極氷床融氷史 : 地形地質学から見た現状と課題

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Please use this identifier to cite or link to this item:http://doi.org/10.14943/lowtemsci.76.227

Title: 最終氷期最盛期以降の南極氷床融氷史 : 地形地質学から見た現状と課題
Other Titles: Geomorphological and geological reconstruction of Antarctic Ice Sheet deglaciation since the Last Glacial Maximum : the current situation and future challenges
Authors: 三浦, 英樹1 Browse this author
Authors(alt): Miura, Hideki1
Keywords: 南極大陸
南極氷床
地形地質学
最終氷期最盛期
融氷史
Antarctica
Antarctic Ice Sheet
geomorphology and geology
Last Glacial Maximum
deglaciation
Issue Date: 31-Mar-2018
Publisher: 低温科学第76巻編集委員会
Journal Title: 低温科学
Journal Title(alt): Low Temperature Science
Volume: 76
Start Page: 227
End Page: 241
Abstract: 南極大陸とその周辺に存在する山地,海岸,海底の地形・地質には,過去の南極氷床の盛衰が様々な形で記録されている.これらの記録は,断片的ではあるが,過去の南極氷床の空間的な分布範囲や拡大・縮小過程,当時の氷床底環境などを復元するうえで,他の地球科学的手法では得ることができない独特のデータを提供する.本稿では,地形地質学的に復元された最終氷期最盛期以降の南極氷床融氷史に関する成果の概要と今後の課題を示す.
The Antarctic Ice Sheet history has been recorded on various sediments and rocks of the mountains, coasts and the ocean floor of Antarctica and its surroundings. Although these geomorphological and geological records are fragmentary, they provide unique data for reconstruction of the spatial expansion range, shrinking process and thermal subglacial environments of the past Antarctic Ice sheet. In this paper, we present the outline of the knowledge and understanding of the Antarctic Ice Sheets at the Last Glacial Maximum (LGM) and their subsequent changes throughout the Holocene.
Type: bulletin (article)
URI: http://hdl.handle.net/2115/70337
Appears in Collections:低温科学 = Low Temperature Science > 第76巻

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