The Mid-Pliocene sea-level conundrum: Glacial isostasy, eustasy and dynamic topography

The Mid-Pliocene sea-level conundrum: Glacial isostasy, eustasy and dynamic topography

Determining eustatic sea level during the Mid-Pliocene warm period (~3.3 to 2.9 Ma) has been a central but elusive goal in the study of past warm climates. Estimates of eustatic sea level based on geologic data span a broad range; variation that we now recognize is due in part to geographically vary...

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Bibliographic Details
Main Authors: Rovere, A., Raymo, M., Mitrovica, J., Hearty, P., O'Leary, Mick, Inglis, J.
Format: Journal Article
Published: Elsevier Science BV 2014
Subjects:
isostasy
dynamic topography
Mid-Pliocene sea level
southeast coast USA
Australia
Republic of South Africa
Online Access:http://hdl.handle.net/20.500.11937/49117

Internet

http://hdl.handle.net/20.500.11937/49117

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