ERC Advanced Grant · 2019
Evolution of the Non-Uniformitarian Earth
The project will use a set of innovative techniques to study the two major events that precede classical, uniformitarian geology. We will search for crystallised remnants of the primordial terrestrial magma ocean and examine the consequences of our observations for mantle dynamics. Crystallisation of the dominant lower mantle phase, bridgmanite, imparts a Mg and Si isotopic fingerprint to cumulates and evolving liquid of the magma ocean. Identifying the relicts of these small but distinctive fractionations requires application of our bespoke, high precision analytical protocols. As an integral part of this work, we will undertake coupled first principles calculations and petrological…
From the public funding record at EU CORDIS. Describes the funded project, not the reviews below.