A5051803365- earthquake and tectonic studies
- Geological and Geophysical Studies Worldwide
- Geology and Paleoclimatology Research
- Geological and Geochemical Analysis
- Geological formations and processes
- Geological and Geophysical Studies
- Landslides and related hazards
- Marine and environmental studies
- Geological and Tectonic Studies in Latin America
- Archaeological and Historical Studies
- Methane Hydrates and Related Phenomena
- Maritime and Coastal Archaeology
- Mediterranean and Iberian flora and fauna
- Archaeological and Geological Studies
- Coastal and Marine Dynamics
- Botanical Research and Chemistry
- High-pressure geophysics and materials
- Tropical and Extratropical Cyclones Research
- Earthquake and Tsunami Effects
- Seismology and Earthquake Studies
- Historical and socio-economic studies of Spain and related regions
- Pacific and Southeast Asian Studies
- Analytical Chemistry and Chromatography
- Disaster Management and Resilience
- Seismic Imaging and Inversion Techniques
Laboratoire Magmas et Volcans
2016-2025
Université Clermont Auvergne
2014-2024
Institut de Recherche pour le Développement
2015-2024
Centre National de la Recherche Scientifique
2015-2024
Hôpital Laveran
2017-2022
Observatoire de Physique du Globe de Clermont-Ferrand
2022
Institut National des Sciences de l'Univers
2021
Clermont Université
2011-2015
Hôpital d'instruction des Armées Desgenettes
2012-2015
Laboratoire de Géographie Physique et Environnementale
2004-2013
Abstract Applying probabilistic methods to infrequent but devastating natural events is intrinsically challenging. For tsunami analyses, a suite of geophysical assessments should be in principle evaluated because the different causes generating tsunamis (earthquakes, landslides, volcanic activity, meteorological events, and asteroid impacts) with varying mean recurrence rates. Probabilistic Tsunami Hazard Analyses (PTHAs) are conducted areas world at global, regional, local scales aim...
Research Article| September 01, 2007 Eruptive and structural history of Teide Volcano rift zones Tenerife, Canary Islands J.C. Carracedo; Carracedo 1Estación Volcanológica de Canarias, Consejo Superior Investigaciones Cientificas, La Laguna, Spain Search for other works by this author on: GSW Google Scholar E. Rodríguez Badiola; Badiola 2Museo Nacional Ciencias Naturales, 28006 Madrid, H. Guillou; Guillou 3Laboratoire des Sciences du Climat et l'Environnement, Commisariat à 3Énergie...
Abstract Numerical modelling of a rapid, partial destabilization Anak Krakatau Volcano (Indonesia) was performed in order to investigate the tsunami triggered by this event. Krakatau, which is largely built on steep NE wall 1883 eruption caldera, active its SW side (towards caldera), makes edifice quite unstable. A hypothetical 0.280 km 3 flank collapse directed southwestwards would trigger an initial wave 43 m height that reach islands Sertung, Panjang and Rakata less than 1 min, with...
Coastal boulder deposits (CBD), transported by waves at elevations above sea level and substantial distances inland, are markers for marine incursions. But whether they tsunami or storm can be difficult to determine. Equations from seminal work Nott (1997), here referred as the Approach, commonly employed calculate nominal wave heights masses, a means discriminate between emplacement mechanisms. Systematic review shows that this approach is based on assumptions not securely founded, direct...
Abstract. The 17 July 2006, a tsunami struck the southern coast of Java, Indonesia, causing over 730 casualties. triggering earthquake located 225 km off Pangandaran (9.222° S, 107.320° E), occurred at 15:19 LT (UTC +7) with 7.7 magnitude on Richter scale (Harward Center and CEA/DAM). In order to calibrate numerical models understand phenomenon, we conducted 6-weeks field survey in August 2006 from Cimerak district West Java Gunung Kidul Central Java. Data collection involved measurements...