RETRACTED: 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

• Published in: Quaternary Research
• Main Authors: Yoo, Kyu-Cheul, Il Yoon, Ho, Park, Byong-Kwon, Kim, Yeadong
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press (CUP) 2006
• Subjects: King George Island; West Antarctica; South Shetland Islands; Marian; Antarc*; Antarctica
• Online Access: http://dx.doi.org/10.1016/j.yqres.2005.07.002; http://api.elsevier.com/content/article/PII:S0033589405001006?httpAccept=text/xml; http://api.elsevier.com/content/article/PII:S0033589405001006?httpAccept=text/plain; https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400013570

Abstract This article has been retracted at the request of the Editor-in-Chief. Please see http://www.elsevier.com/locate/withdrawalpolicy .Reason: Following publication of this article, the Editor-in-Chief has realized that much of the included information had been previously published in the paper Yoon, H.I., Yoo, K.-C., Park, B.-K., Kim, Y., Khim, B.-K., and Kang, C.-Y., 2004. The origin of massive diamicton in Marian and Potter coves, King George Island, West Antarctica. Geosciences Journal 8, 1–10. As a result, the later manuscript is being retracted; readers interested in this topic should refer to the earlier paper.