F. Chambat

ORCID: 0000-0001-8967-077X
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About
Contact & Profiles
Research Areas
  • Geomagnetism and Paleomagnetism Studies
  • Geophysics and Gravity Measurements
  • High-pressure geophysics and materials
  • Astro and Planetary Science
  • earthquake and tectonic studies
  • Seismic Imaging and Inversion Techniques
  • Stellar, planetary, and galactic studies
  • Planetary Science and Exploration
  • Scientific Research and Discoveries
  • Geology and Paleoclimatology Research
  • Geological and Geochemical Analysis
  • Galaxies: Formation, Evolution, Phenomena
  • Computational Physics and Python Applications
  • Astronomy and Astrophysical Research
  • Geophysics and Sensor Technology
  • Analytic Number Theory Research
  • Climate variability and models
  • Mathematics and Applications
  • Oceanographic and Atmospheric Processes
  • Agriculture and Rural Development Research
  • Theoretical and Computational Physics
  • Seismology and Earthquake Studies
  • History and Theory of Mathematics
  • Paranormal Experiences and Beliefs
  • Spacecraft Dynamics and Control

Université Claude Bernard Lyon 1
1996-2024

École Normale Supérieure de Lyon
2005-2024

Centre National de la Recherche Scientifique
2008-2024

Laboratoire de Géologie de Lyon : Terre, Planètes et Environnement
1996-2024

Université Jean Monnet
1996-2023

Laboratoire de Sciences de la Terre
2001-2008

Observatoire astronomique de Strasbourg
1996

Institut de physique du globe de Paris
1994

Université de Strasbourg
1994

The knowledge of the gravitational potential coefficients J2 and J4 a hydrostatic Earth model is necessary to deal with non-hydrostatic properties our planet. They are indeed fundamental parameters when modelling 3-D density structure or rotational behaviour most widely used values computed by Nakiboglu need be updated for two reasons. First, we have noted mistake in one his formulae. Secondly, value inertia ratio I/MR2 chosen at time prem not any more best estimate. Both corrections...

10.1111/j.1365-246x.2010.04771.x article EN Geophysical Journal International 2010-09-24

Abstract On Venus, radar observations of the surface have highlighted two categories craters: bright‐floored, interpreted as pristine, and dark‐floored, being partially filled by lava. While volcanic resurfacing occurs within outside craters in plains, it seems mainly concentrated interior dark‐floored crustal plateaus, suggesting that magma is negatively buoyant there. Indeed, crater unloading may facilitate vertical ascent a decompressing underlying crust. However, topography also...

10.1029/2023je008189 article EN cc-by-nc Journal of Geophysical Research Planets 2024-04-30

10.1016/s0031-9201(01)00200-x article EN Physics of The Earth and Planetary Interiors 2001-08-01

10.1016/j.epsl.2013.12.008 article EN Earth and Planetary Science Letters 2014-01-03

10.1016/j.pepi.2009.04.007 article EN Physics of The Earth and Planetary Interiors 2009-05-10

Context. We investigate the hydrostatic shape and gravitational potential coefficients of self-gravitating rotating bodies large enough to have undergone internal differentiation chemical stratification. Quantifying these properties under assumption equilibrium forms basis for interpreting gravity data in terms interior structure infer deviations from hydrostaticity that can bring information on thermal history objects.

10.1051/0004-6361/201527005 article EN Astronomy and Astrophysics 2015-11-13

Abstract The large trans-Neptunian objects (TNO) with radii larger than 400 km are thought to be in hydrostatic equilibrium. Their shapes can provide clues regarding their internal structures that would reveal information on formation and evolution. In this paper, we explore the equilibrium figures of five TNOs, show difference between homogeneous heterogeneous interior models reach several kilometers for fast rotating low density bodies. Such a could measurable by ground-based techniques....

10.3847/2041-8213/aa95bd article EN The Astrophysical Journal Letters 2017-11-15

We have analysed more than four years of data from the Strasbourg superconducting gravimeter to retrieve period and damping nearly diurnal-free wobble (NDFW). The removal noise spikes is found be crucial for an accurate determination tidal-wave amplitudes phases. A new simple algorithm derived which allows analytical solution NDFW using complex gravimetric factors three resonant diurnal waves. results show a huge reduction confidence intervals when compared with previous investigation...

10.1111/j.1365-246x.1994.tb02127.x article EN Geophysical Journal International 1994-01-01

In a system where two phases coexist, seismic wave can disrupt the pre-existing equilibrium and induce re-equilibration process. Because kinetics of phase change is not instantaneous, transformation induces an attenuation that be quantified using appropriate physical theory. Kinetics Earth′s transitions are well known: in this paper we show they constrained by data. We quantify influence transition upon mode body reflexion coefficient. perform numerical application for olivine to wadsleyite...

10.1111/j.1365-246x.2012.05417.x article EN Geophysical Journal International 2012-03-29

Abstract Condensed planets contract or expand as their temperature changes. With the exception of effect phase changes, this phenomenon is generally interpreted being solely related to thermal expansivity planet’s components. However, changes in density affect pressure and gravity and, consequently, compressibility. A radius also linked its rate rotation. Here again, pressure, gravity, compressibility are coupled. In article we clarify how a condensed planet with rotation, using simple...

10.3847/1538-4357/ad4113 article EN cc-by The Astrophysical Journal 2024-05-30

10.1016/j.pepi.2005.01.002 article EN Physics of The Earth and Planetary Interiors 2005-03-22

We present an approach of the inverse gravimetric problem that allows gravity to be directly related deviatoric stresses without any rheological assumptions. In this a new set parameters is considered: (1) density variations over equipotential surfaces and height interfaces above corresponding (2) stress difference. The method applied lunar topographic data are interpreted in term transversally isotropic within Moon. It also provides inference on crustal thickness variations. estimated...

10.1029/2007je002936 article EN Journal of Geophysical Research Atmospheres 2008-02-01

Aims. A recent major high-angular-resolution imaging survey of 42 large main-belt asteroids ( D > 100 km) with VLT/SPHERE has provided shape models these bodies an unprecedented accuracy. We ask whether the shapes correspond to Maclaurin or Jacobi hydrostatic equilibrium figures. Methods. To address this question, we compared aspect ratios and rotation rates Results. The polar flattenings globally do not match those ellipsoids. Moreover, equatorial axes are compatible axial symmetry as...

10.1051/0004-6361/202346206 article EN cc-by Astronomy and Astrophysics 2023-06-21

Various papers have discussed the forward relationships between internal density anomalies of a planet and its external gravity field. The inverse modelling, i.e. finding from potential is known to be highly non-unique. In this research note, we explain how 3-D basis can built represent variations that includes subset explicitly spans kernel operator. This representation clarifies origin non-uniqueness sources implies existence natural minimal norm for density. We illustrate these ideas by...

10.1111/j.1365-246x.2005.02650.x article EN Geophysical Journal International 2005-06-17

Condensed planets contract or expand as their temperature changes. With the exception of effect phase changes, this phenomenon is generally interpreted being solely related to thermal expansivity planet's components. However, changes in density affect pressure and gravity and, consequently, compressibility. A radius also linked its rate rotation. Here again, pressure, compressibility are coupled. In article we clarify how a condensed planet with rotation, using simple rigorous thermodynamic...

10.48550/arxiv.2404.14278 preprint EN arXiv (Cornell University) 2024-04-22
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