Sequential phreatomagmatic eruptions during the lateral propagation of giant dyke swarms
Giant dyke swarms are widely developed on Earth, Venus and Mars and form by lateral propagation of constituent dykes over 100s to 1000s of kilometres. The failure of these dykes to erupt magma at surface partly accounts for their long-range propagation. However, the lack of preservation of the upper...
| Main Authors: | , , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
Geological Society of America
2024
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