Did Paleogene North Atlantic rift-related eruptions drive early Eocene climate cooling?
The delivery of volcanogenic sulphur into the upper atmosphere by explosive eruptions is known to cause significant temporary climate cooling. Therefore, phreatomagmatic and phreatoplinian eruptions occurring during the final rifting stages of active flood basalt provinces provide a potent mechanism...
| Published in: | Lithos |
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| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
2005
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| Subjects: | |
| Online Access: | https://oro.open.ac.uk/6911/ |