Paleo-environmental and volcano-tectonic evolution of the southeastern flank of Mt. Etna during the last 225 ka inferred from the volcanic succession of the ‘Timpe’, Acireale, Sicily-Reference-Cited by-同舟云学术

Paleo-environmental and volcano-tectonic evolution of the southeastern flank of Mt. Etna during the last 225 ka inferred from the volcanic succession of the ‘Timpe’, Acireale, Sicily

Published:2002-03 Issue:1-2 Volume:113 Page:289-306
ISSN:0377-0273
Container-title:Journal of Volcanology and Geothermal Research
language:en
Short-container-title:Journal of Volcanology and Geothermal Research

Author:

Corsaro Rosa Anna,Neri Marco,Pompilio Massimo

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference47 articles.

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2. Some ultramafic xenoliths from Etna;Aurisicchio;Rend. Soc. It. Mineral. Petrol.,1987

3. Importance of gravitational spreading in the tectonic and volcanic evolution of Mount Etna;Borgia;Nature,1992

4. Origin and evolution of ancient Etnean alkaline volcanics: petrology of lavas and study of fluid and melt inclusions in minerals from a succession exposed on the lower eastern flank;Busà;Plinius,1999

5. Mt. Etna 1991–93 eruption chronology and geological observations;Calvari;Acta Vulcanol.,1994

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