Kennedy, Martin J. - Department of Earth Science, University of California at Riverside

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Kennedy, Martin J. - Department of Earth Science, University of California at Riverside

INTRODUCTION There is a fundamental distinction between
doi:10.1144/0016-76492006-191 2007; v. 164; p. 895-921Journal of the Geological Society
deforming high-molecular-weight glassy poly-mer at 386 K is nearly identical to the penetra-
DOI: 10.1126/science.1088342 , 859 (2003);302Science
The late Precambrian greening of the Earth L. Paul Knauth1
INTRODUCTION Terminal Proterozoic glacial intervals are
Snowball Earth termination by destabilization of equatorial permafrost methane clathrate
Secular changes in the importance of neritic carbonate deposition as a control on the magnitude and stability of Neoproterozoic ice ages
2001 Geological Society of America. For permission to copy, contact Copyright Permissions, GSA, or editing@geosociety.org. Geology; December 2001; v. 29; no. 12; p. 11351138; 1 figure; Data Repository item 2001130. 1135