| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9532510 | Marine Geology | 2005 | 10 Pages |
Abstract
The deepest and stronger velocity anomaly correspond to a basin-wide seismic unconformity (RSU2, Late Miocene-Early Pliocene in age). This anomaly is interpreted as evidence of a major advance of the West Antarctic ice sheet on the continental shelf that resulted in high velocity and low porosity in sediment immediately above the unconformity.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Flavio Accaino, Gualtiero Böhm, Giuliano Brancolini,