Jan Zalasiewicz
University of Leicester, Leicester, N/A
Activity
2006
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WERE TRANSGRESSIVE BLACK SHALES A NEGATIVE FEEDBACK MODULATING GLACIOEUSTASY DURING THE EARLY PALAEOZOIC ICEHOUSE?
T198 Epi-continental Seas in the Geological Record: The Limitations of the Uniformitarian Paradigm IWednesday, 25 October 20068:00 AM - 12:00 PM