The thermal state of Io

Icarus

Volumn 154, Issue 2, 2001, Pages 548-550

  Moore, William B ^a,b  

^a UNIVERSITY OF CALIFORNIA   (United States)

^b UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0035735894     PISSN: 00191035     EISSN: None     Source Type: Journal    
DOI: 10.1006/icar.2001.6739     Document Type: Article

References (16)

1. Basaltic Volcanism on the Terrestrial Planets
2. Shear modulus and Q of forsterite and dunite near partial melting from forced-oscillation experiments
3. Mountains and calderas on Io: Possible implications for lithosphere structure and magma generation
4. Permeability of partially molten upper mantle rocks from experiments and percolation theory
5. Thermal-orbital histories of viscoelastic models of Io (J1)
6. A mathematical model of magma transport in the asthenosphere
7. Revisiting the hypothesis of a mushy global magma ocean in Io
8. Nonlinear pressure diffusion in a porous medium: Approximate solutions with applications to permeability measurements using transient pulse decay method
9. Galileo at Io: Results from high-resolution imaging
10. Magma transport of heat on Io: A mechanism allowing a thick lithosphere
11. The mountains of Io: Global and geological perspectives from Voyager and Galileo
12. Io's thermal emission from the Galileo photopolarimeter-radiometer
13. Mechanics of fluid-rock systems
14. Io's heat flow from infrared radiometry: 1983-1993
15. Permeabilities, interfacial areas and curvatures of partially molten systems: Results of numerical computation of equilibrium microstructures
16. Grain-scale permeabilities of texturally equilibrated, monomineralic rocks