As long as rapid continental weathering continued, carbonate was deposited on the oceanic crust and
subducted into what Lowe calls «a big storage facility... that kept most of the carbon dioxide out of the atmosphere.»
Not exact matches
Often, one plate gets
subducted under another and sinks
into the mantle beneath, while elsewhere, new rocks rise to the surface.
Over long periods of time (think millions of years), the crust is
subducted deep
into the mantle.
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.
It marks the plate boundary between the
subducting Nazca plate and the South America plate, where the oceanic crust and lithosphere of the Nazca plate begin their descent
into the mantle beneath South America.
The intermediate - depth regions of the
subducting Nazca plate can be segmented
into five sections based on their angle of subduction beneath the South America plate.
At subduction zones such as these, an oceanic tectonic plate sinks (
subducts)
into the Earth's interior, the mantle.
More perplexing still, seismic studies have shown no evidence that ocean crust is being
subducted — thrust down
into the hot mantle underlying the trench — which is the process that results in quakes at other deep - sea trenches.
As the
subducting plate sinks deeper
into the earth, it encounters higher and higher temperatures and pressures, which release the significant amount of water trapped in waterrich minerals that exist within the slab.
A numerical simulation shows how Earth's crust (blue) is
subducted and transported
into the mantle (orange).
The scientists believe the
subducted area was absorbed
into Europa's ice shell, which may be up to 20 miles (about 30 kilometers) thick, rather than breaking through it
into Europa's underlying ocean.
Hydration reactions along the
subducting plate are thought to carry water deep
into the Earth, and dehydration reactions at greater depths release fluids
into the overlying mantle that promote melting and volcanism.
Subducted - A geological process in which one edge of a crustal plate is forced sideways and downward
into the mantle below another plate.
Some of the warm water would be
subducted by Atlantic Meridional Overturning Circulation / Thermohaline Circulation, some would be carried by ocean currents
into the Arctic Ocean where it would melt sea ice, and the remainder would be spun southward by the North Atlantic gyre toward the tropics so it could be warmed more by the effects of the slower - than - normal trade winds.
The back radiation which is entrained
into the ocean bulk by wave action is minimal, because wave action
subducts water which is well below the level back radiation can penetrate to (little more than its own wavelength).