CORDIS Project
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This research investigates the fragmentation mechanisms of low viscosity magmas like kimberlite and carbonatite. By analyzing pyroclastic deposits and conducting experiments, the project aims to understand how these magmas behave during explosive eruptions, focusing on their unique physical properties.
The fragmentation mechanisms of low viscosity magmas such as kimberlite and carbonatite remain enigmatic despite comprehensive research on their more silicious counterparts.
In order to understand how and why they erupt we must look at their pyroclastic deposits.
The little that is known about the fragmentation of these low-viscosity magmas suggests that they behave differently to the higher viscosity magmas such as basalts and rhyolites, implying there may be something unique about the physical…
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