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

Author:

Tarff R. W.,Day S. J.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Reference29 articles.

1. Austin-Erickson A, Büttner R, Dellino P, Ort MH, Zimanowski B (2008) Phreatomagmatic explosions of rhyolitic magma: experimental and field evidence. J Geophys Res 113(B11), B11201

2. Bonelli RJ (1950) “Contribucion al estudio de la erupcion del Nambroque o San Juan.” Madrid Inst. Geografico y Catastral 25

3. Cimarelli C, Di Traglia F, Taddeucci J (2010) Basaltic scoria textures from a zoned conduit as precursors to violent Strombolian activity. Geology 38(5):439–442

4. Costa A (2001) Análise do Mercado Energético e potencial de penetracao de Tecnologias Europeias de Energias Renováveis em Cabo Verde. Final Report, THERMIE Type B Action STR/1938/98/PT. European Union, Brussels

5. Day SJ (1996) Hydrothermal pore fluid pressure and the stability of porous, permeable volcanoes. Geol Soc Spec Pub 110:77–93

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