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Publications tagged with [mantle convection]
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<p>Seafloor topography has been a key observational constraint on the thermal evolution of oceanic lithosphere, which is the top boundary layer of convection in Earth's mantle. At least for the first ~70 Myr, the age progression of seafloor depth is known ...
Filed under:
Geology -
General Geology
Reference:
Earth and Planetary Science Letters 268 (2008) 41–51
Coltice N.
,
Phillips B. R.
et al.
This paper shows that continental aggregation promotes large-scale melting without requiring the involvement of plumes.
Filed under:
Geology -
General Geology
Reference:
GEOLOGY, May 20070, v7. 35, no. 5, p. 391-394
