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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.
Article history
first online:
02 Jun 2017
Citation
John C. Behrendt, Alan K. Cooper, Thomas I. Wilch, George H. Denton, William C. McIntosh, Daniel R. Lux; Minimal Pliocene-Pleistocene uplift of the dry valleys sector of the Transantarctic Mountains: A key parameter in ice-sheet reconstructions: Comment and Reply. Geology ; 22 (7): 668–670. doi: https://doi.org/10.1130/0091-7613(1994)022<0668:MPPUOT>2.3.CO;2
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