Is there a conflict between the Neoproterozoic glacial deposits and the snowball Earth interpretation: an improved understanding with numerical modeling
- 1 March 2003
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 208 (1-2) , 101-112
- https://doi.org/10.1016/s0012-821x(02)01152-4
Abstract
No abstract availableKeywords
This publication has 48 references indexed in Scilit:
- Is high obliquity a plausible cause for Neoproterozoic glaciations?Geophysical Research Letters, 2002
- Neoproterozoic glacial-rainout intervals: Observations and implicationsGeology, 2002
- Modeling the evolution of Antarctic ice sheet over the last 420,000 years: Implications for altitude changes in the Vostok regionJournal of Geophysical Research: Atmospheres, 2001
- Vreeland Diamictites - Neoproterozoic glaciogenic slope deposits, Rocky Mountains, northeast British ColumbiaBulletin of Canadian Petroleum Geology, 2000
- Thickness of tropical ice and photosynthesis on a snowball earthGeophysical Research Letters, 2000
- The Sr, C and O isotopic evolution of Neoproterozoic seawaterPublished by Elsevier ,1999
- Two diamictites, two cap carbonates, two δ13C excursions, two rifts: The Neoproterozoic Kingston Peak Formation, Death Valley, CaliforniaGeology, 1999
- Coupling an AGCM with an ISM to investigate the ice sheets mass balance at the Last Glacial MaximumGeophysical Research Letters, 1998
- Paleomagnetic evidence for low-latitude glaciation during deposition of the Neoproterozoic Rapitan Group, Mackenzie Mountains, N.W.T., CanadaCanadian Journal of Earth Sciences, 1997
- An exceptionally thick upper Proterozoic (Sturtian) glacial succession in the Mount Painter area, South AustraliaGSA Bulletin, 1989