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Joint Program in Marine Geology and Geophysics
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Mark D. Behn2 studentsKenneth W. W. Sims2 studentsthe Rayleigh number of the upper mantle is at least 1051 studentbetween 501 studentAnne Cohen1 student55 mW/m2 . This value agrees with measurements of heat flow on old seafloor in the Atlantic. In conclusion1 studentthe heat transport from the longer wavelength convection flattens the depth-age curve1 studentHenry J.B. Dick1 studentJeffrey Donnelly1 studentthe evolution of the surface plates would initially involve small scale convection which is driven by shear coupling to instabilities downstream1 studentRob L. Evans1 studentthe low viscosity zone may also thicken with age. Finally1 studentGregory Hirth1 studentSusan E. Humphris1 studentOliver Jagoutz1 studentRobert S. Detrick Jr Jian Lin1 studentDaniel Lizarralde1 studentto small scale convection associated with fracture zones. This convective flow would begin at close to 5 m.y1 studentwe prefer an approximate model for the viscosity structure of the upper mantle which initially has a 125 km thick low viscosity zone that represents a viscosity contrast of two orders of magnitude. The viscosity contrast decreases as the plate ages to one order of magnitude or less by 130 m.y1 studentDaniel C. McCorkle1 student
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