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Stable isotope analyses of metamorphic minerals to trace fluids in the crust:
Tracing the passage of fluids in rocks in not a trivial matter. Fluids commonly escape the rock leaving behind chemical traces or minute inclusions in the minerals they interacted with. Variations in the isotopic composition of water-soluble elements (such as oxygen and boron) can be used to trace the passage of aqueous fluids. Importantly, using an ion microprobe (e.g. SHRIMP), oxygen and boron isotopes in minerals can be analyzed at the same micro scale as chemical zoning and age, making it possible to reconstruct P-T-time-fluid path from complex metamorphic minerals.
As a group we are working on the measurements of oxygen isotopes in-situ in a range of minerals commonly found in metamorphic rocks.
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crossref(2024)
Michelle Ulrich,Daniela Rubatto,Jorg Hermann, Thorsten A. Markmann,Anne -Sophie Bouvier,Etienne Deloule
CHEMICAL GEOLOGY (2024): 121978
Earth and Planetary Science Letters (2024): 118893
Lithos (2024): 107702
Earth and Planetary Science Letters (2024)
Chemical Geologypp.122060, (2024)
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