Compositional layering in io driven by magmatic segregation and volcanism
The compositional evolution of volcanic bodies like Io is not well understood. Magmatic segregation and volcanic eruptions transport tidal heat from Io's interior to its surface. Several observed eruptions appear to be extremely high temperature (≥1600 K), suggesting either very high degrees of...
Main Authors: | , , , , |
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Format: | Journal article |
Language: | English |
Published: |
Wiley
2020
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