Volcanism and deformation since 12,000 years at the Campi Flegrei caldera (Italy)
- 1 August 1999
- journal article
- Published by Elsevier in Journal of Volcanology and Geothermal Research
- Vol. 91 (2-4) , 221-246
- https://doi.org/10.1016/s0377-0273(99)00037-2
Abstract
No abstract availableKeywords
This publication has 12 references indexed in Scilit:
- The Neapolitan Yellow Tuff, a large-magnitude trachytic phreatoplinian eruption: eruptive dynamics, magma withdrawal and caldera collapsePublished by Elsevier ,2003
- Short-term ground deformations and seismicity in the resurgent Campi Flegrei caldera (Italy): an example of active block-resurgence in a densely populated areaJournal of Volcanology and Geothermal Research, 1999
- The Agnano–Monte Spina eruption (4100 years BP) in the restless Campi Flegrei caldera (Italy)Journal of Volcanology and Geothermal Research, 1999
- The restless, resurgent Campi Flegrei nested caldera (Italy): constraints on its evolution and configurationPublished by Elsevier ,1999
- Averno tuff ring in Campi Flegrei (south Italy)Bulletin of Volcanology, 1994
- Vesuvius/Avellino, one possible source of seventeenth century BC climatic disturbancesNature, 1990
- The 1538 Monte Nuovo eruption (Campi Flegrei, Italy)Bulletin of Volcanology, 1987
- Volcanic hazard assessment in the Phlegraean Fields: a contribution based on stratigraphic and historical dataBulletin of Volcanology, 1984
- A preliminary study of stress pattern at Phlegraean Fields as inferred from focal mechanismsBulletin of Volcanology, 1984
- University of Rome Carbon-14 Dates IXRadiocarbon, 1971