Chilled margin fragmentation as a trigger for transition from Strombolian to phreatomagmatic explosive activity at Cova de Paul Crater, Santo Antao, Cape Verde Islands

Bulletin of Volcanology

Volumn 75, Issue 7, 2013, Pages 1-14

  Tarff, R W ^a   Day, S J ^b  

^a UNIVERSITY OF LONDON   (United Kingdom)

^b UNIVERSITY COLLEGE LONDON   (United Kingdom)

Author keywords

Chilled margins; Fuel coolant interaction; Groundwater; Hydrogeology; Maar; Phreatomagmatic; Strombolian

Indexed keywords

AQUIFER; CLAST; EXPLOSIVE VOLCANISM; FRAGMENTATION; GROUNDWATER FLOW; HYDROGEOLOGY; MAAR; PHREATOMAGMATISM; VESICLE; VOLCANIC ERUPTION;

CAPE VERDE; ITALY; LIPARI ISLANDS; MESSINA [SICILY]; SICILY; STROMBOLI;

EID: 84879054836     PISSN: 02588900     EISSN: 14320819     Source Type: Journal    
DOI: 10.1007/s00445-013-0735-0     Document Type: Article

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