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Research Article| July 01, 1994

Minimal Pliocene-Pleistocene uplift of the dry valleys sector of the Transantarctic Mountains: A key parameter in ice-sheet reconstructions: Comment and Reply

John C. Behrendt;

John C. Behrendt

1

U.S. Geological Survey, MS 964, Federal Center, Denver, Colorado 80225

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Alan K. Cooper;

Alan K. Cooper

2

U. S. Geological Survey, Menlo Park, California 22092

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Thomas I. Wilch;

Thomas I. Wilch

3

Department of Geoscience, New Mexico Institute of Mining and Technology, Socorro, New Mexico 87801

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George H. Denton;

George H. Denton

4

Department of Geological Sciences and Institute for Quaternary Studies, University of Maine, Orono, Maine 04469

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William C. McIntosh;

William C. McIntosh

3

Department of Geoscience, New Mexico Institute of Mining and Technology, Socorro, New Mexico 87801

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Daniel R. Lux

Daniel R. Lux

5

Department of Geological Sciences, University of Maine, Orono, Maine 04469

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Geology (1994) 22 (7): 668–670.

https://doi.org/10.1130/0091-7613(1994)022<0668:MPPUOT>2.3.CO;2

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