The key to sources of the Pliocene and Pleistocene glaciation is at the bottom of the Barents Sea
- 1 May 1978
- journal article
- Published by Springer Nature in Nature
- Vol. 273 (5658) , 138-140
- https://doi.org/10.1038/273138a0
Abstract
No abstract availableKeywords
This publication has 7 references indexed in Scilit:
- Was there a late-Würm Arctic Ice Sheet?Nature, 1977
- The Effects of Changing the Solar Constant on the Climate of a General Circulation ModelJournal of the Atmospheric Sciences, 1975
- Wittfoge's Science of SocietyTelos, 1975
- Stability of the Junction of an Ice Sheet and an Ice ShelfJournal of Glaciology, 1974
- Arctic Ocean Sediments, Microfauna, and the Climatic Record in Late Cenozoic TimePublished by Springer Nature ,1974
- Paleomagnetism of the Port Stanley Till, OntarioGSA Bulletin, 1974
- Paleomagnetic stratigraphy of younger basalts and intercalated plio-pleistocene tillites in IcelandInternational Journal of Earth Sciences, 1964