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...
Published in: | Journal of Geophysical Research: Solid Earth |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
American Geophysical Union
2005
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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 |