![](/images/icons/spacer.gif) |
Detailed Reference Information |
Mound, J.E. and Mitrovica, J.X. (1998). True polar wander as a mechanism for second-order sea-level variations. Science 279(5350): 534-537. |
|
Long-term wander of the rotation pole can be a significant contributor to second-order (time scales of similar to 100 million years) sea-level variations. Numerical predictions based on realistic viscoelastic Earth models and paleomagnetically constrained polar motion yield global-scale, differential sea-level trends that can be as large as similar to 200 meters. From the results presented here, it is argued that the well-documented, second-order, Cretaceous-Tertiary sea-level cycle should be reinterpreted as some combination of a eustatic and a regionally varying rotational signal. |
|
![](/images/icons/spacer.gif) |
![](/images/icons/spacer.gif) |
BACKGROUND DATA FILES |
|
![](../images/icons/sq.gif) |
Abstract![](/images/icons/spacer.gif) |
![](../images/buttons/view.very.flat.gif) |
![](../images/buttons/download.very.flat.gif) |
|
|
|
Keywords
earths rotation, mantle rheology, subduction, continents, plate, fluctuations, pleistocene, topography, viscosity, inversion |
|
Publisher
American Association for the Advancement of Science 1200 New York Avenue NW Washington, DC 20005 1-202-326-6540 1-202-682-0816 webmaster@aaas.org |
|
|
![](/images/icons/spacer.gif) |