t (Myr) 0 50 100 150 200 400 50 600 y (km) 800 100 1000 150 0
- ( ) KX T – To y : erf (8) T1 - To 2 VKx/u where y is the depth, k the thermal diffusivity, x the distance from the ridge, and u the horizontal velocity of the plate. 1 Given k = 1 mm’s-1, and Ti To = 1300 K, calculate the isotherms for T – To = 200, 400, 600, 800, 1000, and 1300 K. Create a plot similar to Figure 4-24 (p. 158) from the book. 1
t (Myr) 0 50 100 150 200 400 50 600 y (km) 800 100 1000 150 0 - ( ) KX T – To y : erf (8) T1 - To 2 VKx/u where y is t
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t (Myr) 0 50 100 150 200 400 50 600 y (km) 800 100 1000 150 0 - ( ) KX T – To y : erf (8) T1 - To 2 VKx/u where y is t
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