Postspreading rifting in the Adare Basin, Antarctica: Regional tectonic consequences

Abstract

[1] Extension during the middle Cenozoic (43–26 Ma) in the north end of the West Antarctic rift system (WARS) is well constrained by seafloor magnetic anomalies formed at the extinct Adare spreading axis. Kinematic solutions for this time interval suggest a southward decrease in relative motion between East and West Antarctica. Here we present multichannel… (More)

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Cite this paper

@inproceedings{Granot2010PostspreadingRI, title={Postspreading rifting in the Adare Basin, Antarctica: Regional tectonic consequences}, author={Ron Granot and Steve Cande and Joann Stock and F. J. Davey and R. W. Clayton}, year={2010} }