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Projekt Druckansicht

Diffusive Fraktionierung von Lithium- und Borisotopen in Silikatschmelzen: ein Werkzeug zur Untersuchung von Entgasungsprozessen in aufsteigenden Magmen

Antragsteller Professor Dr. Max Wilke
Fachliche Zuordnung Mineralogie, Petrologie und Geochemie
Förderung Förderung von 2017 bis 2021
Projektkennung Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 349804343
 
Erstellungsjahr 2022

Zusammenfassung der Projektergebnisse

In this study the diffusivity and kinetic fraction of Li and B in a rhyolitic melt composition was determined for H2O-contents that are quite typical for natural magmas. These data do fill a gap in knowledge and clearly document the strong effect of H2O dissolved in silicate melts on the transport kinetics of these two elements. Based on these results, time windows for ascent-speedometers could be established that range from seconds to hours for Li, and from hours to weeks or months for B, depending on H2O-content of the melt. By decompression experiments with various decompression rates the evolution of Li and B contents and isotopes during bubble nucleation and growth was determined and provided insights to realistic situations of natural magma ascent and eruption and the chemical variations around vesicles that can be expected. With these data the predictive quality of numerical models on the chemical evolution of degassing and ascending magmas was assessed to point out their strengths and limits.

Projektbezogene Publikationen (Auswahl)

 
 

Zusatzinformationen

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