Magma flow localisation during dyke propagation produces complex magma transport pathways
Abstract Basaltic fissure eruptions, the most common type of eruption on Earth, are fed by dykes, which are magma-filled cracks that propagate through the crust. It is well-established that dykes have a segmented structure, but the impact of this structural complexity on the development of magma flo...
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| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2025-07-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/s41467-025-61620-5 |
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