Tectonic evolution of the west Scotia Sea

Joint inversion of isochron and flow line data from the flanks of the extinct West Scotia Ridge spreading center yields five reconstruction rotations for times between the inception of spreading prior to chron C8 (26.5 Ma), and extinction around chron C3A (6.6–5.9 Ma). When they are placed in a regi...

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Bibliographic Details
Published in:Journal of Geophysical Research: Solid Earth
Main Authors: Eagles, Graeme, Livermore, Roy A., Fairhead, J. Derek, Morris, Peter
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2005
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/1750/
http://www.agu.org/pubs/crossref/2005/2004JB003154.shtml
https://doi.org/10.1029/2004JB003154