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Convection and Macrosegregation in Magma Chambers
1992Magmas accumulate in large reservoirs where convection occurs, driven by density differences due to fractional crystallization and temperature variations. The observations consist of igneous rocks representing the final crystallized product and volcanic lava series.
S. R. Tait, C. Jaupart
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No single model for supersized eruptions and their magma bodies
Nature Reviews Earth & Environment, 2021Colin J N Wilson +2 more
exaly
Zoned magma chambers: the influence of magma chamber geometry on sidewall convective fractionation
Journal of Volcanology and Geothermal Research, 1995S.L.de Silva, J.A. Wolff
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