Eruptive activity of the Santorini Volcano controlled by sea-level rise and fall
Sea-level change is thought to influence the frequencies of volcanic eruptions on glacial to interglacial timescales. However, the underlying physical processes and their importance relative to other influences (for example, magma recharge rates) remain poorly understood. Here we compare an approxim...
| Príomhchruthaitheoirí: | , , , , , , , , |
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| Formáid: | Journal article |
| Teanga: | English |
| Foilsithe / Cruthaithe: |
Springer Nature
2021
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