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Field observations and seismic reflection surveys suggest that this missing material has been downfaulted. The volume of the caldera infill is estimated as 18\u201326 km\n                    <jats:sup>3<\/jats:sup>\n                    dense rock equivalent (DRE), increasing the total of the Minoan eruption deposits to 78\u201386 km\n                    <jats:sup>3<\/jats:sup>\n                    DRE and making it the largest known Holocene eruption. This study highlights a general mechanism whereby caldera eruption volumes could be significantly underestimated.\n                  <\/jats:p>","DOI":"10.1144\/jgs2013-113","type":"journal-article","created":{"date-parts":[[2014,6,10]],"date-time":"2014-06-10T03:01:42Z","timestamp":1402369302000},"page":"583-590","source":"Crossref","is-referenced-by-count":69,"title":["Revised estimates for the volume of the Late Bronze Age Minoan eruption, Santorini, Greece"],"prefix":"10.1144","volume":"171","author":[{"given":"E. 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