The Neoproterozoic (1000–540 Ma) glacial intervals: No more snowball earth?
about
Low-latitude glaciation and rapid changes in the Earth's obliquity explained by obliquity-oblateness feedback.Paleomagnetic Constraints on Neoproterozoic ‘Snowball Earth' Continental ReconstructionsImpact of ocean dynamics on the simulation of the neoproterozoic “snowball Earth”Paleomagnetism of the Paleoproterozoic Gowganda and Lorrain formations, Ontario: low paleolatitude for Huronian glaciationBiogeographic analyses of the Ediacara biota: a conflict with paleotectonic reconstructionsProterozoic (pre-Ediacaran) glaciation and the high obliquity, low-latitude ice, strong seasonality (HOLIST) hypothesis: Principles and tests
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The Neoproterozoic (1000–540 Ma) glacial intervals: No more snowball earth?
description
im Mai 1994 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
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наукова стаття, опублікована в травні 1994
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name
The Neoproterozoic (1000–540 Ma) glacial intervals: No more snowball earth?
@en
The Neoproterozoic
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type
label
The Neoproterozoic (1000–540 Ma) glacial intervals: No more snowball earth?
@en
The Neoproterozoic
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prefLabel
The Neoproterozoic (1000–540 Ma) glacial intervals: No more snowball earth?
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The Neoproterozoic
@nl
P1476
The Neoproterozoic (1000–540 Ma) glacial intervals: No more snowball earth?
@en
P2093
Rob van der Voo
P356
10.1016/0012-821X(94)90253-4
P407
P577
1994-05-01T00:00:00Z
P819
1994E&PSL.123....1M