2010 - Fabrizio Serra Editore
Artículo
Digital Version
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The Deep-sea Flanks of the Stromboli Island Volcano : Survey Techniques and Research Results
P. 91-94
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Información
ISSN: 1724-0425
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En el mismo archivo
- Foreword
- Present-day Kinematics and Recent Evolution of the Calabrian Arc : the Contribution of Large Gps Network Analysis
- Petrochemical Contributions to the Understanding of Geology and Volcano Behaviour of Stromboli
- Structural Framework of the Stromboli Volcano, Lateral Collapses and the Dyke System
- Present-day Activity of Stromboli : Eruptive History and Eruptive Styles
- Shallow Feeding System : Contributions from Texture and Mineral Chemistry
- Magma Degassing, Crystallization and Eruption at Stromboli : Messages of Olivine Crystals and of Their Melt Inclusions
- The Deep Feeding System of Stromboli : Constraints from Experimental Petrology
- Geophysical Evidence of Strombolian Activity
- Description and Chronology of the 2002-2003 and 2007 Eruptions
- Monitoring Eruptive Activity Through Web-cameras Network and Thermal Mapping
- Shallow Dike Emplacement and Related Hazard in Central Stratovolcanoes
- Petrologic Monitoring of Lavas and Pyroclasts Erupted from Stromboli Volcano
- Volcanic Degassing at Stromboli : Insights from Plume Observations
- Geochemistry of Stromboli Discharged Fluids
- Ground Deformation Monitoring Techniques and Applications to Mt. Etna and Stromboli Volcanoes
- Ground Deformation Modeling and Recent Applications to Mt. Etna and Stromboli Eruptions
- Monitoring Deformations of the Sciara del Fuoco (Stromboli) Through Ground-based Radar Interferometry
- The Stromboli VLP Seismic Activity : Monitoring Techniques and Research Results
- Monitoring the 2007 Eruption by an Integrated Geophysical Network
- Multibeam Bathymetry for Studying Volcanic Flank Morphology and Mass Failure : Examples from Stromboli 2002 and 2007 Eruptions
- The Deep-sea Flanks of the Stromboli Island Volcano : Survey Techniques and Research Results
- The December 2002 Stromboli Tsunami : an Accidental Occurrence or a Structural Source of Hazard?
- Modelling the Dynamics of Volcanic Systems
- Civil Protection Preparedness and Response to the 2002-2003 and 2007 Eruptive Crises
- Eruptive Scenario of Ash-dominated Events at Vesuvius : the AP3 Eruption (2,710 ± 60 years bp)
- Past and Recent Instability in the South-western Flank of Irazu Volcano (Costa Rica)
- List of Participants
