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200 Myr of oceanic crust accumulation

Shear-driven magma segregation. Super-adiabatic boundary layer. REGION B. Hawaii source. Thermal max. 300 km. Tp decreases with depth. Narrow downwellings. Broad passive upwellings. MORB source. TRANSITION ZONE (TZ). 600 km. 600 km. (RIP). 200 Myr of oceanic crust accumulation.

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200 Myr of oceanic crust accumulation