There it will seek out new species and habitats; it may also study subduction zones,
where oceanic crust is recycled back into the earth's mantle.
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.
It's the first time this tectonic process has been discovered beneath land; all other known subduction zones occur underwater
where oceanic crusts meet.
Not exact matches
Generally speaking, there are two types of
crust on Earth: a lighter continental
crust that is rich in silicon and constitutes the dry land above sea level, and a denser
oceanic crust where water gathers in the form of large oceans.
Its strength resulted from the abrupt release of plate tectonic forces, a process known as subduction, centered on an area beneath Honshu
where it slides over the top of
oceanic crust.
In high - pressure and high - temperature X-ray measurements that were partly conducted at DESY, scientists created conditions similar to those in so - called subduction zones
where an
oceanic plate dives under the continental
crust.
Older
crust in turn is then forced back down into the Earth's mantle in places
where a continental plate meets an
oceanic plate.