The combination of a hotter mantle and denser rocks likely
caused subducting plates to sink all the way to the bottom of the mantle, 2,800 kilometers below the surface, forming a «graveyard» of slabs atop the Earth's core.
Not exact matches
While this would have steadily sunk into the mantle, it would not have
caused the soft lithosphere to
subduct and tear and therefore would not have produced plate margins.
The heat and stress
causes some of the material on the
subducting plate to become a buoyant mineral called serpentinite that rises and erupts out of mud volcanoes.
Water migrates upwards and
causes the top of the
subducted oceanic crust to melt, producing magma beneath the Cascade volcanoes.
The CO2 tectonic source grew from 60 to 50 Myr BP as India
subducted carbonate - rich ocean crust while moving through the present Indian Ocean prior to its collision with Asia about 50 Myr BP [8],
causing atmospheric CO2 to reach levels of the order of 1000 ppm at 50 Myr BP [9].
Specifically, during the period 60 My BP (60 million years before present) to 50 My BP India was plowing north rapidly (20 cm per year) through the Tethys Ocean and in the process
subducting carbonate - rich ocean crust,
causing atmospheric CO2 to increase.