Приклади вживання Subduction zones Англійська мовою та їх переклад на Українською
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The Hadean and Archean subduction zones.
Water in subduction zones recycles back to Earth's surface.
The areas where this happens are called subduction zones.
In subduction zones, earthquakes occur at depths as great as 700 km.
The Pacific Plate became active in subduction zones.
Subduction zones occur when one or both of the tectonic plates are composed of oceanic crust.
However, the rock forms from subduction zones all around the world.
The most notorious tsunamigenic earthquakes occur at subduction zones.
On Earth, subduction zones produce continental crust, which can protrude from the ocean(the continents).
Andesite rocks will form in regions above subduction zones.
The destruction of oceanic crust occurs at subduction zones where oceanic crust is forced under either continental crust or oceanic crust.
These plates are destroyed by subduction into the mantle at subduction zones.
The broad, curving scarp resembles some of Earth's subduction zones where crustal plates are pushed over each other.
These"greenstones" are similar to thesediments today found in oceanic trenches, above subduction zones.
Also, we would thus expect the trenches adjacent to the subduction zones today to be filled with undisturbed late-Flood and post-Flood sediments.
Unlike other subduction zones on Earth, Cascadia presently experiences low levels of seismicity and has not generated a megathrust earthquake since January 26, 1700.
Earth appears to be the only terrestrial planet with subduction zones and plate tectonics.
Subduction zones experience various types of earthquakes(or seismicity); including slow earthquakes, megathrust earthquakes, interplate earthquakes, and intraplate earthquakes.
Earth appears to be the only terrestrial planet with subduction zones and plate tectonics.
Despite low levels of seismicity compared to other subduction zones, Cascadia hosts various types of earthquakes that are recorded by seismic and geodetic instruments, such as seismometers and GNSS receivers.
In the 1980s, geophysicists Tom Heaton and Hiroo Kanamori of Caltechcompared the generally quiet Cascadia to more active subduction zones elsewhere in the Ring of Fire.
It is possible that diamonds can form from coal in subduction zones and in meteoroid impacts, but diamonds formed in this way are rare and the carbon source is more likely carbonate rocks and organic carbon in sediments, rather than coal.
In the next phase of organic andinorganic carbon on the ocean floor sank into the mantle in subduction zones, where oceanic plate dives under the continental and melts.
As a result, the planet was much more geologically active,processes like convection and plate tectonics occurred much faster, and subduction zones were more common.
Because plate tectonics drivesoceanic plates back down into the mantle at subduction zones, there is no oceanic crust or sediment older than 180 million years for us to examine.
Slow slip events were discovered in the Cascadia Subduction Zone in the U.S. Pacific Northwest in the early 2000s,shortly before they were spotted in New Zealand's subduction zones, says Rebecca Bell.
The western border is a convergent boundarylargely responsible for the mountains in western Sulawesi, subduction zones also exist on the eastern border near Seram and the southern border with the Timor Plate.
In the south and the southwest, it has a convergent border with the African plate which is shown in features of the compression of an oceanic cover near the Mediterranean Sea, and also within a continental cover of Anatoly,and also in subduction zones along the Greek and Cyprian arches.
Prior to the 1980s, scientists thought that the subduction zone did not generate earthquakes like other subduction zones around the world, but research by Brian Atwater and Kenji Satake tied together evidence of a large tsunami on the Washington coast with documentation of an orphan tsunami in Japan(a tsunami without an associated earthquake).
At the next stage, organic and inorganic carbon at thebottom of the ocean was immersed in the mantle in subduction zones, where oceanic plates dive under the continental and melt.