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Showing 1–4 of 4 results

Advanced filters: Author: Stephan Klemme Clear advanced filters

Halogen abundance evidence for the formation and metasomatism of the primary lunar crust

Formation and metasomatism of the Moon’s primary crust constrained by experimentally determined partition coefficients for chlorine coupled with models of the evolution of the lunar interior.

Jie-Jun Jing
Jasper Berndt
Wim van Westrenen
ResearchOpen Access20 Jun 2025
Nature Communications

Volume: 16, P: 1-10
Reply to: Silica is unlikely to be soluble in upper crustal carbonatite melts

Jasper Berndt
Stephan Klemme
ResearchOpen Access21 Feb 2023
Nature Communications

Volume: 14, P: 1-3
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
Origin of carbonatites—liquid immiscibility caught in the act

Carbonatites are fascinating igneous rocks and their genesis remains enigmatic. Here the authors show that a Ca-rich carbonatite melt formed by liquid immiscibility from a phonolitic magma of the Laacher See volcano in the Eifel, Germany.

Jasper Berndt
Stephan Klemme
ResearchOpen Access24 May 2022
Nature Communications

Volume: 13, P: 1-8