Evolution of magma decompression and discharge during a Plinian event (Late Bronze-Age eruption, Santorini) from multiple eruption-intensity proxies
Author:
Funder
Directorate for Geosciences
Clermont Université
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology
Link
http://link.springer.com/content/pdf/10.1007/s00445-021-01438-3.pdf
Reference61 articles.
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2. Biass S, Bonadonna C (2011) A quantitative uncertainty assessment of eruptive parameters derived from tephra deposits: the example of two large eruptions of Cotopaxi volcano, Ecuador. Bull Volcanol 73:73–90. https://doi.org/10.1007/s00445-010-0404-5
3. Bonadonna C, Costa A (2013) Plume height, volume, and classification of explosive volcanic eruptions based on the Weibull function. Bull Volcanol 75:742. https://doi.org/10.1007/s00445-013-0742-1
4. Bond A, Sparks RSJ (1976) The Minoan eruption of Santorini, Greece. J Geol Soc 132:1–16. https://doi.org/10.1144/gsjgs.132.1.0001
5. Cadoux A, Scaillet B, Druitt TH, Deloule E (2014) Magma storage conditions of Large Plinian eruptions of Santorini volcano (Greece). J Petrol 55:1129–1171. https://doi.org/10.1093/petrology/egu021
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