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Articles
Drift of Continental Rafts with Asymmetric Heating
1 Department of Physics and Institute of Geophysics, University of California, Los Angeles 90024
A laboratory model of a lithospheric raft is propelled through a viscous asthenospheric layer with constant velocity of scaled magnitude appropriate to continental drift. The propulsion is due to differential heat concentration in the model oceanic and continental crusts.
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Science. ISSN 0036-8075 (print), 1095-9203 (online)