Construct · 1 fields · 1 citations

strain-rate magma fragmentation criterion: a standalone construct

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Volcanology

the condition that magma breaks into fragments when its deformation rate exceeds the rate at which the melt can relax as a viscous liquid.

In volcanology, strain-rate magma fragmentation criterion refers to the condition that magma breaks into fragments when its deformation rate exceeds the rate at which the melt can relax as a viscous liquid. This meaning comes from Papale (1999) in Nature.[1]

Unit
Recovery means
Measured by

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Nearby constructs

condition2 fields · 2 citationsjingle · one word, two constructs fragmentation5 fields · 5 citationsjingle · one word, five constructs

References

Papale, P. (1999). Strain-induced magma fragmentation in explosive eruptions. Nature, 397(6718), 425-428. https://doi.org/10.1038/17109

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