Presents the principles of convection in the earth's mantle in an accessible style.This problem is left as an Exercise. ... with an observed heat flux of about 90mW/ m2 for lithosphere of this age, and a mean heat flux of about 100 mW/m2 for the whole sea floor. ... would not be 10 times greater, but 102/3 = 4.6 times greater.
|Author||:||Geoffrey Frederick Davies|
|Publisher||:||Cambridge University Press - 1999-11-18|