Life of the Bellingshausen plate

The onset of independent Bellingshausen plate movement in the South Pacific is estimated at just after chron C33o. This event closely follows a change in the offset sense on the transform arm of the Late Cretaceous Pacific-Phoenix-Antarctic triple junction and accompanies the creation and/or lengthe...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Eagles, Graeme, Gohl, Karsten, Larter, Robert D.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2004
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/12154/
https://nora.nerc.ac.uk/id/eprint/12154/1/2003GL019127.pdf
http://www.agu.org/journals/gl/gl0407/2003GL019127/index.html
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Summary:The onset of independent Bellingshausen plate movement in the South Pacific is estimated at just after chron C33o. This event closely follows a change in the offset sense on the transform arm of the Late Cretaceous Pacific-Phoenix-Antarctic triple junction and accompanies the creation and/or lengthening, by different mechanisms, of long-offsets on the Pacific-Antarctic ridge at the Udintsev, Tharp, Heezen and V transforms, as the triple junction stepped away from the ridge. At around chron C27, the Bellingshausen plate ceased to move independently and the Pacific-Antarctic ridge inherited the set of long offset transforms. Shortly afterwards, the gravity fabric on the flanks of much of the ridge displays evidence for a spreading rate decrease possibly related to transpression on the long-offset transforms. We speculate on a link between these events and regional tectonic changes around chron C27.