CORDIS Project
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This research investigates the role of saline fluids in the formation of natural diamonds and kimberlite rocks. By conducting high-pressure experiments, it aims to provide insights into the geological processes that create these valuable resources.
The majority of natural diamonds that have great economic importance for the gem industry are formed at great depth beneath old continents in the subcontinental lithospheric mantle (SCLM).
The main carrier of these diamonds are kimberlites, deep volcanic rocks that transport fragments of the SCLM to the Earth’s surface.
Both diamond formation and kimberlite genesis are still heavily debated processes in the Geosciences.
Growing evidence from natural samples, such as fluid inclusions in diamonds,…
UNIVERSITAET MUENSTER
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