Geologists and many other geographically centered scientists
have argued for decades over how the process of plate tectonics had initially
evolved. Recently, Jeroen van Hunen, a geophysicist at Durham University in England worked
with Jean-François Moyen, of Jean Monnet University in Saint-Etienne, France to
give us their theories. A model was
developed showing how one plate of earth's thin crust subducts below another.
The theory thus far has
supported a continuous process where plates converge at boundary points, and
are famously based on movement fuelled by temperature and/or substrate mass and
density (i.e dense continental crust v. the lighter basaltic rock of oceanic
crust). Some theories in the past have
been maintained by evidence of rocks surfaced from mantle regions of the lithosphere
and have supported more of a continuous motion of plates at boundaries
resulting in subduction (Fig 2.1).
Fig. 2.1 - subduction zone of two plates
photo credit:. Web. 2 May 2012. <volcanoes.usgs.gov>
Moyen and Hunen found rocks striated with pristine rocks
layered with altered rock in Zimbabwe and Southern Australia that account for
more of a 'start and stop' method of initially forming our modern day plate
tectonics. The discussion follows one
of geothermal interest and spotlights convection loops. The two scientists did their study showing
their audiences how changes as few as 200 degrees higher, would cause crust to
break off and interrupt the continuous flow theory. It would take time for the layer to cool
enough to begin re-subduction which if anything but a good argument, supports
how the ancient rock striations in Zimbabwe have been aligned as they are.
References
Witze, Alexandra. "Stop-and-go plate tectonics." Science News 9 Apr. 2012. Web. 2 May 2012. <http://www.sciencenews.org/view/generic/id/339797/title/Stop-and-go_plate_tectonics>.
Arbogast, Alan F. Discovering Physical Geography. second ed. Hoboken: John Wiley and Sons, 2011. 355-59. Web. 22 Apr. 2012.
Glasscoe, Maggi. History of Plate Tectonics. N.p., n.d. Web. 17 Mar. 2012. <http://scign.jpl.nasa.gov/learn/plate2.htm>.
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