Heat transport by variable viscosity convection II: pressure influence, non-Newtonian rheology and decaying heat sources

Physics of the Earth and Planetary Interiors

Volumn 37, Issue 2-3, 1985, Pages 183-205

  Christensen, Ulrich R ^a,b  

^a Inst fur Meteorologie und Geophysik   (Germany)

^b MAX PLANCK INSTITUTE FOR CHEMISTRY   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0022182762     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/0031-9201(85)90051-2     Document Type: Article

References (18)

1. Thermal convection with strongly temperature dependent viscosity
2. Convection in a variable-viscosity fluid: Newtonian versus power-law rheology
3. Heat transfer by variable viscosity convection and implications for the Earth's thermal evolution
4. Convection with pressure- and temperature-dependent non-Newtonian rheology
5. Convection with decaying heat sources: constant viscosity
6. Steady-state secondary convection beneath lithospheric plates with temperature- and pressure-dependent viscosity
7. Subducted slabs and geoid: constraints on mantle rheology and flow
8. Convection, composition and the thermal state of the lower mantle
9. Material properties for mantle convection consistent with observed surface fields
10. Low stress high temperature creep of olivine single crystals
11. The effect of pressure on the dislocation recovery in olivine
12. Dynamic support of the outer rise
13. Thermal convection in non-Newtonian fluids: volumetric heating and boundary layer scaling
14. Studies of finite amplitude non-Newtonian thermal convection with application to convection in the Earth's mantle
15. Glacial isostatic adjustment
16. Viscosity-depth profile in the Earth's mantle effects of polymorphic phase transitions
17. Cooling of the Earth—a constraint on palaeotectonic hypotheses
18. The viscosity of the lower mantle as inferred from rotational data