scholarly article | Q13442814 |
P819 | ADS bibcode | 1995JGR...10012731P |
P356 | DOI | 10.1029/95JB01078 |
P2093 | author name string | W. Richard Peltier | |
Giovanni Pari | |||
P2860 | cites work | Melting of (Mg, Fe)SiO3-Perovskite to 625 Kilobars: Indication of a High Melting Temperature in the Lower Mantle | Q33295570 |
Preliminary reference Earth model | Q55868389 | ||
Satellite gravity measurements and a laminar viscous flow model of the Earth's mantle | Q56852898 | ||
Intermittent layered convection in a model mantle with an endothermic phase change at 670 km | Q59051540 | ||
Effects of an endothermic phase transition at 670 km depth in a spherical model of convection in the Earth's mantle | Q59056430 | ||
Surface deformation, gravity anomalies and convection | Q59938542 | ||
Seismic constraints on mantle flow and topography of the 660-km discontinuity: evidence for whole-mantle convection | Q60066282 | ||
An inversion for radial viscosity structure using seismic tomography | Q60714427 | ||
Thermal expansivity in the lower mantle | Q107275412 | ||
Thermal expansion measurements at very high pressure, systematics, and a case for a chemically homogeneous mantle | Q107275447 | ||
P433 | issue | B7 | |
P921 | main subject | aquatic science | Q4782809 |
P304 | page(s) | 12731-12751 | |
P577 | publication date | 1995-07-10 | |
P1433 | published in | Journal of Geophysical Research | Q2738009 |
P1476 | title | The heat flow constraint on mantle tomography-based convection models: Towards a geodynamically self-consistent inference of mantle viscosity | |
P478 | volume | 100 |
Q70641667 | A carbon cycle coupled climate model of Neoproterozoic glaciation: Influence of continental configuration on the formation of a “soft snowball” |
Q107275360 | Effect of the mid-mantle viscosity and phase-transition structure on 3D mantle convection |
Q107269091 | Layered convection and the impacts of the perovskite-postperovskite phase transition on mantle dynamics under isochemical conditions |
Q56384479 | Postglacial variations in the level of the sea: Implications for climate dynamics and solid-Earth geophysics |
Search more.