Richard F Katz 1, Rolf Ragnarsson 2 and Eberhard Bodenschatz 2,3
1
Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
2
Laboratory of Atomic and Solid State Physics, Cornell University, Ithaca, NY, USA
3
Max Planck Institute for Dynamics and Self-Organization, Göttingen, Germany
Richard F Katz et al 2005 New J. Phys. 7 37
Rotating, growing microplates are observed in a wax analogue model of sea-floor spreading. Wax microplates are kinematically similar to sea-floor tectonic microplates in terms of spreading rate and growth rate. Furthermore, their spiral pseudofault geometry is quantitatively consistent with Schouten's oceanic microplate model. These results suggest that Schouten's edge-driven microplate model captures the kinematics of tectonic microplate evolution on Earth. Based on the wax observations, a theory for the nucleation of overlapping spreading centres, the precursors of tectonic microplates, is developed.
91.50.Ey Ocean bottom processes
65F35 Matrix norms, conditioning, scaling (See also 15A12, 15A60)
Issue 1 (January 2005)
Received 21 November 2004
Published 1 February 2005
Richard F Katz et al 2005 New J. Phys. 7 37