Thermal Constraints on the Longevity, Depth, and Vertical Extent of Magmatic Systems
Abstract Magmatic regions are typically viewed as vertical systems, with magma coming in the bottom and either freezing in the crust to form plutons or erupting to form volcanic rocks. Maintaining an upper‐crustal magmatic system for 105–106 Ma timescales requires establishing and maintaining a stro...
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| Format: | Article |
| Language: | English |
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Wiley
2021-04-01
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| Series: | Geochemistry, Geophysics, Geosystems |
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| Online Access: | https://doi.org/10.1029/2020GC009459 |