G
Glenn W. Berger
Researcher at Desert Research Institute
Publications - 59
Citations - 2862
Glenn W. Berger is an academic researcher from Desert Research Institute. The author has contributed to research in topics: Thermoluminescence dating & Radiocarbon dating. The author has an hindex of 30, co-authored 59 publications receiving 2723 citations. Previous affiliations of Glenn W. Berger include Western Washington University.
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Journal ArticleDOI
Late Quaternary slip rates across the central Tien Shan, Kyrgyzstan, central Asia
Stephen C. Thompson,Stephen C. Thompson,Ray J. Weldon,Charles M. Rubin,Kanatbek E Abdrakhmatov,Peter Molnar,Peter Molnar,Glenn W. Berger +7 more
TL;DR: In this article, slip rates across active faults and folds show that late Quaternary faulting is distributed across the central Tien Shan, not concentrated at its margins, suggesting that deformation is concentrated along major fault zones near range-basin margins.
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The last glacial maximum in central and southern North Island, New Zealand: a paleoenvironmental reconstruction using the Kawakawa Tephra Formation as a chronostratigraphic marker
Brad Pillans,Matt S. McGlone,Alan Palmer,Dallas C. Mildenhall,Brent V. Alloway,Glenn W. Berger +5 more
TL;DR: The Kawakawa Tephra Formation, comprising Oruanui Ignimbrite flow member and Aokautere Ash airfall member, represents the products of an exceptionally large and widespread volcanic eruption from Taupo Volcanic Centre in the North Island of New Zealand.
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Neotectonics of the Min Shan, China: Implications for mechanisms driving Quaternary deformation along the eastern margin of the Tibetan Plateau
Eric Kirby,Kelin X. Whipple,B. Clark Burchfiel,Wenqing Tang,Glenn W. Berger,Zhiming Sun,Zhiliang Chen +6 more
TL;DR: In this article, the authors exploit the preservation of a series of variably deformed Quaternary sediments along the western flank of the mountain range to investigate the Pleistocene-Holocene deformation field within the Min Shan region.
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Initiation and development of the Laurentide and Cordilleran Ice Sheets following the last interglaciation
Peter U. Clark,John J. Clague,B. Brandon Curry,Aleksis Dreimanis,Stephen R. Hicock,Gifford H. Miller,Glenn W. Berger,Nicholas Eyles,Michel Lamothe,Banks Miller,Robert J. Mott,R.N. Oldale,R.R. Stea,J.P. Szabo,L. H. Thorleifson,J.-S. Vincent +15 more
TL;DR: Fossil records from sites overridden by or adjacent to the Laurentide Ice Sheet indicate that the climate of the last interglaciation (Oxygen-Isotope Substage 5e, ca. 130-116 ka) was warmer than today.