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The Last Glacial Maximum and deglaciation in southern South America
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In the citing paper
“The LGM in southern Patagonia is estimated around 26 000 yr BP, but the beginning of significant glacial retreat occurred between 21 000 and 17 000 yr BP (Hulton et al., 2002;Hein et al., 2010;Glasser et al., 2011;Davies and Glasser, 2012;Moreno et al., 2015;Bendle et al., 2017;Reynhout et al., 2019;Davies et al., 2020).”
From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Hulton et al., 2002
In the citing paper
“The Patagonian Ice Sheet covered the southern Patagonian Andes between ∼ 47 000 and ∼ 17 000 yr BP, extending from latitudes 38 to 55° S with an estimated area of ∼ 490 000 km 2 (Fig. 1a); volume of ∼ 550 000 km 3 ; and average and maximum thickness of 1100 and 2500 m, respectively, based on preserved glacial geomorphology, stratigraphy, palaeoecology, and geochronological data (Moreno et al., 199”
From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Hulton et al., 2002
In the citing paper
“The LGM in southern Patagonia is estimated around 26 000 yr BP, but the beginning of significant glacial retreat occurred between 21 000 and 17 000 yr BP (Hulton et al., 2002;Hein et al., 2010;Glasser et al., 2011;Davies and Glasser, 2012;Moreno et al., 2015;Bendle et al., 2017;Reynhout et al., 2019;Davies et al., 2020).”
From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Hulton et al., 2002
In the citing paper
“As a result, previous models have assumed simple deglaciation histories as well”
From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Hulton et al., 2002
In the citing paper
“Tracing back the post-LGM or Holocene ice loss rate from current measurements is difficult considering that climate was at least 6 °C colder during the LGM”
From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Hulton et al., 2002
In the citing paper
“it is difficult to position in time present-day uplift rate measurements within the investigated deglaciation scenarios to assess the contribution of post-LGM, post-LIA, and present-day deglaciation to the maximum uplift rate budget.”
From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Hulton et al., 2002
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Metadata
- Authors
- Hulton, N. R. J., Purves, R. S., McCulloch, R. D., Sugden, D. E., & Bentley, M. J.
- Affiliations
- University of Edinburgh (GB)
- Durham University (GB)
- Corresponding author
- Hulton, N.R.J
- Venue
- Quaternary Science Reviews
- Publisher
- Elsevier BV
- Published
- 2002-01
- Volume
- 21
- Issue
- 1-3
- Pages
- 233-241
- ISSN
- 0277-3791 (ISSN-L)
- OpenAlex
- W1994451395
- Cited by
- 362
- References
- 28
- Citations by year
- 2026: 10 · 2025: 9 · 2024: 22 · 2023: 30 · 2022: 36 · 2021: 16 · 2020: 23 · 2019: 8 · 2018: 20 · 2017: 14 · 2016: 15 · 2015: 13 · 2014: 12 · 2013: 9 · 2012: 24
- FWCI
- 4.71
- Type
- journal article
- Language
- en
- Open access
- Licence
- Locations
- Quaternary Science Reviews (publishedVersion)
- Stirling Online Research Repository (University of Stirling) (submittedVersion)
- Durham Research Online (Durham University) (submittedVersion, cc-by)
- Funders
- Carnegie Trust for the Universities of Scotland
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Cryospheric studies and observations
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
- Keywords
- Last Glacial Maximum, Patagonian Ice Sheet, deglaciation, ice sheet modeling, ice volume, ice mass balance, ice velocity, fjords, global sea level change, Holocene warming, Andes
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