Was the Late-glacial advance at ~14.0 ka B.P. in Torres del Paine (Patagonia, 51S) the most extensive glacial pulse of Oxygen Isotope Stage 2?
- ADS bibcode
- 2010AGUFMGC21A0860G
- year
- 2010
- Listed Authors
- Garcia, J.
- Hall, B. L.
- Kaplan, M. R.
- Schaefer, J. M.
- Vega, R. M.
- Schwartz, R.
- Finkel, R. C.
- Listed Institutions
- Department of Earth Sciences/Climate Change Institute, University of Maine, Orono, ME, USA
- Department of Earth Sciences/Climate Change Institute, University of Maine, Orono, ME, USA
- Geochemistry, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
- Geochemistry, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
- Instituto de Geociencias, Universidad Austral de Chile, Valdivia, Chile
- Geochemistry, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
- Cams, Lawrence Livermore National Laboratory, Livermore, CA, USA
Linked Authors [?]
Linked Institutions