HelioWebUniverse, Time-Frequency, Interfaces, Nanostructures, Atmosphere and Environment, Molecules, Besancon
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- Tidal Disruption of Primordial Planetary Bodies
- Observations of Jupiter Supporting the New Horizons Encounter and During a Period of "Global Upheaval"
- Change in Mediterranean Hydrologic Cycle at Time of Heinrich Events From a High Resolution Multiproxy Record of the Last 50 kyr
- Frictional Properties of Fault Gouges Recovered from NanTroSEIZE Expedition 316 Drilling
- Segmentation of the southern part of the Outer Hebrides Fault Zone (NW Scotland). Implications on the seismotectonic behaviour of large-scale crustal faults
- Debris Field of the July 19, 2009, Impact in Jupiter and Its Long-term Evolution
- Rapid Climatic Variability in the Western Mediterranean during the Last 25,000 Years from the High Resolution Pollen Record ODP Site 976
- STRAIN LOCALIZATION DUE TO RHEOLOGICAL HETEROGENEITY ACROSS A CRUSTAL-SCALE INTRACONTINENTAL SHEAR ZONE
- Thermal Evolution and Composition of the July 2009 Jupiter Impact Site from 7-25 Micron Imaging and Spectroscopy
- Thermal and Near-Infrared Structural Evolution of the 2009 Wesley Jupiter Impact from 1.5-24.5 Micron Imaging
- Calcium isotopic compositions as tracers of vegetation activity in boreal permafrost ecosystems (Kulingdakan watershed, Central Siberia)
- Condensates from stellar protoplanetary nebulae: Implications for heavy element and volatile enrichment in extrasolar planets
- Contribution to the Holocene North Atlantic wind activity reconstruction from Lake Igaliku, South Greenland
- Potential of calcium isotopes to identify fractionations in vegetation: experimental approach
- The role of methanol on the crystallization of Titan's primordial ocean
- Origin of multiple serpentinization events in New Caledonia
- P-T conditions of deformation: A key to understand the mechanical behavior of a thrust fault (Monte perdido thrust fault, Spain)
- Tectonics, Climate, and Mountain Topography
- A new three-dimensional method of fault reactivation analysis
- Comparative Characterization of Extrasolar Super-Earths - Interiors, Atmospheres, and Formation Conditions
- Evolving Deformation Style and Rheology During Transpressive Segmentation and Uplift of Continental Lower Crust
- CO2-SO2 clathrate hydrate formation on early Mars
- Effects of Exoplanet Planetesimal Carbon Chemistry on Habitability
- How can fluid overpressures be developed and maintained in crustal fault zones ?
- Implications of the Nitrogen Isotope Ratio in Titan's Atmosphere for the Nitrogen Ratio in Ammonia in Comets
- Is hyperspectral imaging a possible new approach for fire reconstruction?
- Studying the Formation, Evolution, and Habitability of the Galilean Satellites
- Upward extension of the Nankai accretionary prism megasplay fault into slope basin strata. Insights from drilling at IODP Expedition 338 Site C0022
- Evolution of Continental Lower Crust Recorded By an Exhumed Deep Crustal Intracontinental Shear Zone
- Hydrological Dynamics, Fire History and Carbon Accumulation in the Last Millennium in Western Siberia Reconstructed from a High Resolution Ombrotrophic Peat Archive
- The Redox Dynamics of Iron in a Seasonally Waterlogged Forest Soil (Chaux Forest, Eastern France) Traced with Rare Earth Element Distribution Patterns
- Did high Neo-Tethys subduction rates contribute to early Cenozoic warming?
- Dissolution on Titan and on Earth: Towards the Age of Titan's Karstic-like Landscapes
- Isotopes and Minor Volatiles in the Coma of Comet 67P/Churyumov-Gerasimenko Observed by the Rosetta/ROSINA Instrument: Planetary Implications
- Assimilation of ambient seismic noise in hydrological models allows estimation of hydraulic conductivity in unsaturated media
- Colours of the Outer Solar System Origins Survey (Col-OSSOS): New Insights into Kuiper belt Surfaces
- Dipping Upper Mantle Interface Beneath The North Tanzania Divergence from Receiver Functions
- The North Tanzania Rift seen from multi geophysical tools: link between seismicity and resistivity
- Expert Assessment of Past and Future Changes in Global Fire Regimes