Megacrystals track magma convection between reservoir and surface
International audience Active volcanoes are typically fed by magmatic reservoirs situated within the upper crust. The development of thermal and/or compositional gradients in such magma chambers may lead to vigorous convection as inferred from theoretical models and evidence for magma mixing recorde...
Published in: | Earth and Planetary Science Letters |
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Main Authors: | , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2015
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Subjects: | |
Online Access: | https://hal-insu.archives-ouvertes.fr/insu-01124396 https://hal-insu.archives-ouvertes.fr/insu-01124396/document https://hal-insu.archives-ouvertes.fr/insu-01124396/file/Moussallam-EPSL-2015.pdf https://doi.org/10.1016/j.epsl.2014.12.022 |