Melt inclusion vapour bubbles: the hidden reservoir for major and volatile elements
Swetha Venugopal1,2, Federica Schiavi3, Severine Moune3,4,5
1Department of Earth Sciences, Simon Fraser University, Burnaby, Canada. swethav@sfu.ca.
Scientific Reports
|June 5, 2020
Summary
Reheating melt inclusions (MIs) can alter their volatile content, creating new phases within bubbles. Analyzing only the glass underestimates the original magma composition and storage parameters.
Area of Science:
- Geochemistry
- Volcanology
- Petrology
Background:
- Olivine-hosted melt inclusions (MIs) are crucial for studying magmatic liquids and volatiles.
- Post-entrapment modifications can alter MI glass and bubble compositions.
- Reheating is used to reverse MI crystallization, but its effect on volatiles is debated.
Purpose of the Study:
- To investigate the impact of reheating on volatile and fluid phases within melt inclusions.
- To assess compositional changes in bubbles of both re-heated and naturally glassy MIs.
- To determine if analyzing glass alone underestimates original magma composition.
Main Methods:
- Analysis of crystallised and glassy basaltic MIs.
- Raman spectroscopy for fluid and solid phase identification.
- 3D imaging to study bubble contents before and after re-heating.
Main Results:
- Reheating MIs causes diffusion of elements, forming new phases (SO2, gypsum, Fe-sulphides) within bubbles.
- Naturally glassy MIs also contain solid phases (carbonates, sulphates, sulphides) sequestering significant volatiles (S, CO2, FeO).
- Bubbles in both types of MIs sequester elements, leading to a 'loss' from the glass.
Conclusions:
- Reheating significantly alters MI volatile content and bubble composition.
- Melt inclusion bubbles act as sinks for key magmatic components.
- Glass analysis alone provides an incomplete picture of magma composition and storage.
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