El límite Cuenca Powell/Mar de Weddell. Estructura y relación con la fragmentación Cenozoica de la Península Antàrtica
Late Paleogene to Neogene continental fragmentation of the Northern Antarctic Peninsula caused the development of small oceanic-floored basins such as Powell Basin. On the basis of MCS profiles and swath bathymetry collected during Hesant 92/93 cruise, a tectonic map of the transition zone between P...
Main Authors: | , , , , |
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Format: | Article in Journal/Newspaper |
Language: | Spanish |
Published: |
Sociedad Geológica de España
1996
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Subjects: | |
Online Access: | http://hdl.handle.net/10272/12466 |