Institut de physique du globe de Paris
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Seismotectonic analog experiments: simulating subduction earthquake cycles at laboratory scale
Discussion autour du film "Anthropocène, l’implacable enquête"
The influence of crustal stress on the pathways and evolution of magmas
Fault creep: what is it, how do we find it and what does it mean?
Volcanisme sous-marin : le cas de Mayotte
Oasis de vie au fond des océans et émergence de la vie sur Terre
Missions spatiales et retours d’échantillons
Volcanoes: Earth's angriest yet generous vents
Volcano monitoring from satellite imagery
The shape of the Himalayan “Arc”: an Ellipse pinned by syntaxial strike-slip fault tips
Extrusion tectonics, where do we stand 40 years later?
Continental (and institutional) collision and the evolution of the Tibetan Plateau
Continental deformation and mantle convection, from rifting to collision
The differential tectonic deformation and limited extrusion model of the Qinghai-Tibetan Plateau
How do the continents deform? Evidence from high-resolution geodetic imaging
Welcome and introductory talk
Reconstructing paleoearthquakes from lacustrine sedimentary archives along the Bulnay fault system
Insights into the Sumatran subduction zone & its hazards since 2004 Indian Ocean earthquake& tsunami
Intraplate paleoseismicity in low seismic settings of Central Europe (Germany)
Introductory talk
Why Do Great Continental Transform Earthquakes Nucleate on Branch Faults?
Opportunities and challenges in the use of quaternary dating methods
Aseismic deformation within fold-and-thrust belts
Marine Active Tectonics: Legacy of Paul Tapponnier
Bridging Worlds: From Natural Hazard Assessment to Energy Exploration - Multi-Scale Data Integration
Transient lakes & catastrophic outburst floods in the Kashmir Valley & relationship to mega-quakes
Fault interaction and post-seismic transient in northern Tibet
Active tectonics- recent progress and pending questions
What rock transformations can we detect in geophysical images? The case of the Alps
Pyrenean landscape evolution controlled by postorogenic normal faults