Hostname: page-component-78c5997874-g7gxr Total loading time: 0 Render date: 2024-11-14T09:29:55.740Z Has data issue: false hasContentIssue false
  • English
  • Français

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 online by Cambridge University Press:  20 January 2017

Kyu-Cheul Yoo ,
Ho Il Yoon ,
Byong-Kwon Park  and
Yeadong Kim
Kyu-Cheul Yoo
Affiliation:
Polar Research Institute of Korea Ocean Research and Development Institute, Ansan P.O. Box 29, 425-600 Seoul, Korea
Ho Il Yoon*
Affiliation:
Polar Research Institute of Korea Ocean Research and Development Institute, Ansan P.O. Box 29, 425-600 Seoul, Korea
Byong-Kwon Park
Affiliation:
Polar Research Institute of Korea Ocean Research and Development Institute, Ansan P.O. Box 29, 425-600 Seoul, Korea
Yeadong Kim
Affiliation:
Polar Research Institute of Korea Ocean Research and Development Institute, Ansan P.O. Box 29, 425-600 Seoul, Korea
*
*Corresponding author. Fax: +82 31 408 5825.Email Address:hiyoon@kordi.re.kr(H.I. Yoon).
Get access Rights & Permissions [Opens in a new window]

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This article has been retracted at the request of the Editor-in-Chief.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.

Type
Original Articles
Information
Quaternary Research , Volume 65 , Issue 1 , January 2006 , pp. 57 - 69
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)