CORDIS Project
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This project investigates the recycling of oceanic crust materials in the Earth's mantle and their impact on magma formation. It focuses on the behavior of lithium and boron during the subduction process to better understand intra-plate magmas.
Subduction of oceanic lithosphere back into the Earth's interior is a major geological process and causes heterogeneities in the Earth's mantle.
Once incorporated in the convecting mantle, the recycled crustal material can be re-melted in source regions of intra-plate magmas, which thus plays an important role in the long-time mass flux through different parts of our planet.
In order to track recycled components in intra-plate magmas and to constrain their exact nature, the light lithophile elem…
THE UNIVERSITY OF EDINBURGH
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