Source of Ash Zone 1 in the North Atlantic
Geochemical evidence shows that the silicic component of the widespread Ash Zone 1 in the North Atlantic is derived from a major ignimbrite-forming eruption which occurred at the Katla caldera in southern Iceland during the transition from glacial to interglacial conditions in Younger Dryas time. Bo...
Published in: | Bulletin of Volcanology |
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Main Authors: | , , , , |
Format: | Text |
Language: | unknown |
Published: |
DigitalCommons@URI
1995
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Subjects: | |
Online Access: | https://digitalcommons.uri.edu/gsofacpubs/1081 https://doi.org/10.1007/BF00298704 |