The influence of 5000 year-old and younger glacial mass variability on present-day crustal rebound in the Antarctic Peninsula
Open Access
- 1 November 2000
- journal article
- Published by Springer Nature in Earth, Planets and Space
- Vol. 52 (11) , 1023-1029
- https://doi.org/10.1186/bf03352325
Abstract
No abstract availableThis publication has 27 references indexed in Scilit:
- Postglacial rebound at the northern Cascadia subduction zoneQuaternary Science Reviews, 2000
- Crustal structure of the Filchner‐Ronne Shelf and Coats Land, Antarctica, from gravity and magnetic data: Implications for the breakup of GondwanaJournal of Geophysical Research, 1999
- The BIFROST project: GPS determined 3-D displacement rates in Fennoscandia from 800 days of continuous observations in the SWEPOS networkTectonophysics, 1998
- Glacial and marine geological evidence for the ice sheet configuration in the Weddell Sea–Antarctic Peninsula region during the Last Glacial MaximumAntarctic Science, 1998
- Antarctic glacial history since the Last Glacial Maximum: an overview of the record on landAntarctic Science, 1998
- Predictions of Antarctic crustal motions driven by present‐day ice sheet evolution and by isostatic memory of the Last Glacial MaximumJournal of Geophysical Research, 1998
- Late Holocene palaeoclimatic records from lake sediments on James Ross Island, AntarcticaPalaeogeography, Palaeoclimatology, Palaeoecology, 1996
- The response of large ice sheets to climatic changePhilosophical Transactions Of The Royal Society B-Biological Sciences, 1992
- Modeling the Growth and Decay of the Antarctic Peninsula Ice SheetQuaternary Research, 1989
- The Cenozoic subduction history of the Pacific margin of the Antarctic Peninsula: ridge crest–trench interactionsJournal of the Geological Society, 1982