Research news on oceanic lithosphere

Oceanic lithosphere is the rigid outer shell of Earth underlying ocean basins, comprising oceanic crust and the uppermost mantle, mechanically coupled and behaving as a coherent tectonic plate segment. It forms at mid-ocean ridges through decompression melting of the mantle, producing basaltic crust overlying a lithospheric mantle that cools, thickens, and increases in density with age and distance from the ridge. Its thermal and mechanical structure controls plate flexure, isostasy, and patterns of seismicity, and it ultimately returns to the mantle at subduction zones, playing a central role in plate tectonics, mantle convection, and global geochemical cycling.

New deep-sea measurements show how the ocean floor forms

The first-known direct observations of a seafloor spreading event at a mid-ocean ridge in the Indian Ocean are presented in Nature. The observations offer insight into how new oceanic crust is created.

'Out-of-place' rocks reveal how a young ocean formed

Deep below the Tyrrhenian Sea offshore Italy, scientists drilled into what they thought would be dark mantle rock—and found pieces of granite that seemingly had no business being there. Those unexpected intrusions turned ...

How our planet's history was shaped when the Earth moved

The history of Earth is written on the great tablets of tectonic plates. The motions of plates shaped land masses, formed oceans, and created the varied climates and habitats that set the stage for evolution and the diversity ...

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