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Advanced filters: Author: Remco C. Hin Clear advanced filters

Magnesium isotope evidence that accretional vapour loss shapes planetary compositions

The measurement of magnesium isotope ratios at improved accuracy suggests that planetary compositions result from fractionation between liquid and vapour, followed by vapour escape during accretionary growth.

Remco C. Hin
Christopher D. Coath
Tim Elliott
Research28 Sept 2017
Nature

Volume: 549, P: 511-515
Titanium-rich basaltic melts on the Moon modulated by reactive flow processes

Petrological reaction experiments and magnesium isotope data suggest that reactive flow with mantle cumulates can explain the composition of Ti-rich basaltic magmas.

Martijn Klaver
Stephan Klemme
Tim Elliott
ResearchOpen Access15 Jan 2024
Nature Geoscience

Volume: 17, P: 118-123
Molybdenum systematics of subducted crust record reactive fluid flow from underlying slab serpentine dehydration

Fluid liberation and migration from subducted oceanic slabs play a critical role in arc magmatism but the volume and origin of the released fluids is unclear and difficult to trace. Here, the authors use Molybdenum isotope ratios to tackle these problems.

Shuo Chen
Remco C. Hin
Tim Elliott
ResearchOpen Access21 Oct 2019
Nature Communications

Volume: 10, P: 1-9