Using advanced computer simulations, researchers have reconstructed the geological past of the region, uncovering a ...
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Live Science on MSNScientists discover giant blobs deep inside Earth are 'evolving by themselves' — and we may finally know where they come fromGiant regions of the mantle where seismic waves slow down may have formed from subducted ocean crust, a new study finds.
A breakthrough study has provided the most detailed 3D look yet at the inner workings of the Tonga Subduction Zone, where ...
Deep within Earth’s mantle lie two enormous, continent-sized structures known as LLVPs. Scientists once believed these ...
Giant regions of the mantle where seismic waves slow down may have formed from subducted ocean crust, a new study finds.
Continent-size islands deep inside Earth's mantle could be more than a billion years old, a new study finds. Known as large low-seismic-velocity provinces (LLSVPs), these blobs are both hotter and ...
Beneath the Indian Ocean lies a 106-meter gravity hole, caused by ancient mantle plumes and vanished oceans. Scientists trace ...
Scientists have revealed that two continent-size regions in Earth's deep mantle have distinctive histories and resulting chemical composition, in contrast to the common assumption they are the same.
High-Resolution Anisotropic Tomography Reveals Mantle Flow Complexity and Slab-Plume Interactions, Redefining Subduction Zone ...
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