Results 241 to 250 of about 950,902 (294)

Exploring exoplanet dynamics with JWST: Tides, rotation, rings, and moons. [PDF]

Proc Natl Acad Sci U S A
Millholland SC, Winn JN.
europepmc   +1 more source

Graphite lubricates Mercury's global contraction. [PDF]

Nat Commun
Vergara Sassarini NA, Massironi M, Tesei T, Bistacchi A.   +3 more
europepmc   +1 more source

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The Planetary Interior

2020
exaly   +3 more sources

Rheology (Planetary Interior)

2011
Frank Sohl, Vlada Stamenkovic
exaly   +2 more sources

Stability of Planetary Interiors

Geophysical Journal International, 1969
Summary Many accept thermal convection within the mantle of the Earth as the driving mechanism for continental drift. It is also of considerable interest to determine whether thermal convection is occurring within Venus, Mars, and the Moon. In this paper a systematic treatment of the stability of planetary interiors is given.
G. Schubert, D. L. Turcotte, E. R. Oxburgh   +2 more
openaire   +1 more source

Physics of planetary interiors

Physics of the Earth and Planetary Interiors, 1985
G H A Cole 1984 Bristol: Adam Hilger xiv + 206 pp price £9.95 (paperback) (IOP members' price £7.95) ISBN 0 85274 445 5 A planet, unlike any ordinary star, is a 'cold' body in the sense that its size would not change substantially on being cooled to absolute zero.
  +4 more sources

Interior Structure, Planetary

2011
Models of the interior structure of a ▶ planet or ▶ satellite give the variations of thermodynamic state variables as functions of radius (starting at the center) or depth (starting at the surface). The thermodynamic state variables are pressure, temperature, density (or specific volume), and the concentration of chemical species.
openaire   +1 more source

The Rheology of the Planetary Interior

Journal of Rheology, 1984
The mantle of the earth is rheologically similar to an amorphous polymer. The short‐time‐scale behavior in shear is anelastic and rather well described by a constant Q absorption band. The long‐time‐scale behavior is essentially Newtonian viscous and this mode of deformation dominates the material behavior for times in excess of a Maxwell time which is
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Compressibility and planetary interiors

Physics of the Earth and Planetary Interiors, 1972
Important confirmations that the Earth's inner core is solid have recently come from analyses of records of free Earth oscillations and from the apparent detection of the seismic phase PKJKP. Corresponding support is given to the theory which supplied the primary evidence for rigidity in the inner core.
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Planetary seismology and interiors

Reviews of Geophysics, 1979
The placing of the first seismometer on the Moon by the Apollo 11 astronauts in 1969 started the field of planetary seismology. In the following years five other seismic stations were established on the Moon. The seismic network was operated continuously until all of the ALSEP stations were turned off on 1 October 1977.
openaire   +1 more source