CORDIS Project
Funding breakdown and partner intelligence are Premium
Sign in and upgrade to Premium for EU contribution totals, consortium analytics, OpenAlex research context, and AI summaries. · 0 consortium intelligence fields visible of 1
Start free • Cancel anytime • 14-day refund guarantee
This project focuses on understanding the behavior of fluid silicates under extreme conditions to unravel the Earth's chemical evolution. It aims to develop a comprehensive thermodynamic model of silicate melting and reaction processes, providing insights into the early Earth and magma ocean dynamics.
Partial melting of silicates dominates the chemical evolution of Earth today and was even more important in Earth’s earlier history.
The Earth may have begun in a completely molten state, a global magma ocean, with silicate liquid extending from a dense silicate atmosphere to the boundary with the iron-rich core at a pressure of 140 GPa.
Deep melt may exist in the Earth today, and the magma ocean may have left signatures of its presence.
However, these signals are still uninterpretable becaus…
Partner organizations (coordinator is shown above), with normalized type and CORDIS activity type. Guests see up to 4 partners.
Similar projects, consortium collaboration history, frequent partners, and OpenAlex research context.
Guests see up to 5 EuroSciVoc fields.
Guests see up to 5 topics.
