Plate subduction and collision zone is one of the most active tectonic regimes on the Earth, which controls the mass and energy circulation between the Earth’s surface and interior, produces the ...

Their research has revealed that in the present day, deep below the Earth's surface, the Neotethys oceanic plate—the ocean floor that used to be between the Arabian and Eurasian continents—is ...

I recently participated in a three-week-long, National Science Foundation-funded research cruise to the Mariana Trench. Our ...

The Alps preserve abundant oceanic blueschists and eclogites that exemplify the selective preservation ... Whereas none of the subducted fragments were returned during the first half of the subduction ...

Their findings reveal that, deep beneath the Earth’s surface, the Neotethys oceanic plate—once the seafloor between the Arabian and Eurasian continents—is currently breaking off in a horizontal ...

These movements, called convection, are responsible for plate tectonics. Oceanic plates, being denser, plunge into the mantle at subduction zones, while hot material rises to the surface. This cycle ...

These ancient buried "super-continents"—known to scientists as large low-seismic-velocity provinces (LLSVPs)—were found lurking below Africa and the Pacific Ocean, entombed some 1,200 miles below the ...

These crustal collisions occur gradually over millions of years, yet have a profound impact in reshaping the Earth's surface.