Research news on plate divergence

Plate divergence is a tectonic phenomenon in which lithospheric plates move apart along divergent plate boundaries, driven primarily by mantle convection, slab pull, and ridge push forces. This separation promotes decompression melting of the underlying asthenosphere, generating mafic magmas that ascend to form new oceanic crust at mid-ocean ridges or intraplate rift systems on continents. The process is characterized by extensional stress fields, normal faulting, and symmetric seafloor spreading, often accompanied by linear volcanic and seismic activity. Plate divergence plays a central role in lithosphere recycling, global heat loss, and the long-term evolution of ocean basins and continental configurations.

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 ...

Expedition to Hess Rise in the Northwest Pacific begins

Located in the middle of the North Pacific, between Japan and Canada, lies one of the world's largest oceanic plateaus, the so-called Hess Rise. The plateau is roughly T-shaped and extends over a length of about 1,000 kilometers. ...

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