Приклади вживання Oceanic crust Англійська мовою та їх переклад на Українською
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The oceanic crust.
He characterized thin oceanic crust.
At this type of boundary new oceanic crust is formed in the gap between two diverging plates.
Formation of lithospheric plates and oceanic crust.
When both of the plates are made of oceanic crust, convergence is associated with island arcs such as the Solomon Islands.
Uchytel I., Kapochkin B. Classification of high-speed deformation of the oceanic crust Download.
The Tethys oceanic crust.
The composition of the continental crust is more diverse and thicker than the oceanic crust.
The Permian oceanic crust.
Subduction zones occur when one orboth of the tectonic plates are composed of oceanic crust.
Here two plates move laterally past each other and oceanic crust is neither created nor destroyed.
This takes place at convergent plate boundaries if one orboth of the tectonic plates at the boundary is made of oceanic crust.
So this right here is… actually let me do the oceanic crust in blue, but this is not water, this is rock.
Oceanic crust is also part of tectonic plates, but it is denser than continental lithosphere, so it floats low on the mantle.
A last remnant of Paleo-Tethys Ocean might be an oceanic crust under the Black Sea.
Oceanic crust is additionally a part of tectonic plates, nevertheless it is denser than continental lithosphere, so it floats lower to the mantle.
During periods when continents move apart, more oceanic crust is formed by volcanic activity.
Drilling into the oceanic crust of the mid-ocean ridges has also revealed that those smooth patterns are not present at depth in the actual rocks.
Thus the problem of the historical relationships between the continental and oceanic crust is far from being solved.
Occurs at mid-ocean ridges where new oceanic crust is formed through volcanic activity and then gradually moves away from the ridge.
It's estimated that as much as two-thirds ofEarth's total prokaryote biomass lives within oceanic crust, but very little is known about them.
The destruction of oceanic crust occurs at subduction zones where oceanic crust is forced under either continental crust or oceanic crust.
The plates maybe up to 70 km thick if composed of oceanic crust or 150 km incorporating continental crust. .
Conversely, old oceans dye when continents collide, and the oceanic crust under their pressure sinks back into the mantle.
However, it is thought that it was basaltic in composition, like today's oceanic crust, because little crustal differentiation had yet taken place.
Because young volcanic crust is relatively hotter andless dense than old oceanic crust, the ocean floors rise during such periods.
A powerful magnitude 9.0 earthquakeJapan has led to the release of methane from oceanic crust to the east of the island- along with the microorganisms living in the cortex.