The Neoproterozoic (1000–540 Ma) glacial intervals: No more snowball earth?
- 1 May 1994
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 123 (1-3) , 1-13
- https://doi.org/10.1016/0012-821x(94)90253-4
Abstract
No abstract availableKeywords
This publication has 33 references indexed in Scilit:
- Stromatolites and earth—sun—moon dynamicsPublished by Elsevier ,2003
- Neoproterozoic glaciation in the Broken Hill area, New South Wales, AustraliaGSA Bulletin, 1992
- Paleomagnetism of the Callander Complex and the Cambrian apparent polar wander path for North AmericaCanadian Journal of Earth Sciences, 1991
- Sinian paleomagnetic results from the Tarim block, western ChinaPrecambrian Research, 1991
- Palaeomagnetic data, late precambrian magnetostratigraphy and tectonic evolution of Eastern ChinaPrecambrian Research, 1985
- Paleomagnetism of Late Proterozoic rocks, Victoria Island, Northwest Territories, CanadaCanadian Journal of Earth Sciences, 1983
- Radiations and extinctions of plankton in the late Proterozoic and early CambrianNature, 1982
- Paleomagnetism of late Precambrian to early Paleozoic mixtite-bearing formations in Namibia (South West Africa); the Nama Group and Blaubeker FormationAmerican Journal of Science, 1980
- Non-Synchroneity of Late Precambrian Glaciations in AfricaThe Journal of Geology, 1977
- Laurentide Ice Sheet: Estimated volumes during Late WisconsinReviews of Geophysics, 1972