Retraction of &quot;Advance of the outlet glaciers during regional warming as inferred from Late Holocene massive diamicton in the King George Island fjords, the South Shetland Islands, West Antarctica&quot; [Quaternary Research 65 (2006) 57–69]

Kyu-Cheul Yoo; Ho Il Yoon; Byong-Kwon Park; Yeadong Kim

doi:10.1016/j.yqres.2007.07.015

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Retraction of "Advance of the outlet glaciers during regional warming as inferred from Late Holocene massive diamicton in the King George Island fjords, the South Shetland Islands, West Antarctica" [Quaternary Research 65 (2006) 57–69]

Volume 69, Issue 3
Kyu-Cheul Yoo, Ho Il Yoon, Byong-Kwon Park and Yeadong Kim
DOI: https://doi.org/10.1016/j.yqres.2007.07.015

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Retraction of "Advance of the outlet glaciers during regional warming as inferred from Late Holocene massive diamicton in the King George Island fjords, the South Shetland Islands, West Antarctica" [Quaternary Research 65 (2006) 57–69]

Volume 69, Issue 3
Kyu-Cheul Yoo, Ho Il Yoon, Byong-Kwon Park and Yeadong Kim
DOI: https://doi.org/10.1016/j.yqres.2007.07.015

To save this article to your Google Drive account, please select one or more formats and confirm that you agree to abide by our usage policies. If this is the first time you used this feature, you will be asked to authorise Cambridge Core to connect with your Google Drive account. Find out more about saving content to Google Drive.

Retraction of "Advance of the outlet glaciers during regional warming as inferred from Late Holocene massive diamicton in the King George Island fjords, the South Shetland Islands, West Antarctica" [Quaternary Research 65 (2006) 57–69]

Volume 69, Issue 3
Kyu-Cheul Yoo, Ho Il Yoon, Byong-Kwon Park and Yeadong Kim
DOI: https://doi.org/10.1016/j.yqres.2007.07.015

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Retraction of "Advance of the outlet glaciers during regional warming as inferred from Late Holocene massive diamicton in the King George Island fjords, the South Shetland Islands, West Antarctica" [Quaternary Research 65 (2006) 57–69]

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Retraction of "Advance of the outlet glaciers during regional warming as inferred from Late Holocene massive diamicton in the King George Island fjords, the South Shetland Islands, West Antarctica" [Quaternary Research 65 (2006) 57–69]

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