CORDIS Project
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This project investigates the processes of melting in the Earth's mantle, focusing on the Ronda peridotite in southern Spain. It aims to analyze isotopic variations in mantle-derived melts to understand the behavior of different elements during partial melting.
The mantle is the main source of the magmas that extrude at the Earth surface and an essential goal for Earth scientists is to understand how this reservoir works and how it produces different types of melts.
The isotopic variability of mantle-derived melts reflects the lithological heterogeneity of their source, but provides little information on how these heterogeneities were acquired.
The Ronda peridotite (southern Spain) is a unique natural laboratory to unravel how the mantle acts during me…
CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE CNRS
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