scholarly article | Q13442814 |
P819 | ADS bibcode | 2005JGRE..110.4009V |
P356 | DOI | 10.1029/2004JE002271 |
P2093 | author name string | O. Verhoeven | |
P2860 | cites work | Internal structure and early thermal evolution of Mars from Mars Global Surveyor topography and gravity | Q28138138 |
Global distribution of crustal magnetization discovered by the mars global surveyor MAG/ER experiment | Q28142679 | ||
Fluid core size of Mars from detection of the solar tide | Q38494151 | ||
Interior structure and seasonal mass redistribution of Mars from radio tracking of Mars Pathfinder | Q38502415 | ||
Preliminary reference Earth model | Q55868389 | ||
An inquiry into the lunar interior: A nonlinear inversion of the Apollo lunar seismic data | Q56534263 | ||
A variational approach to the theory of the elastic behaviour of multiphase materials | Q56656594 | ||
Lunar seismology: The internal structure of the Moon | Q56802239 | ||
SNC meteorites: Clues to Martian petrologic evolution? | Q57319609 | ||
Density profile of an SNC model Martian interior and the moment-of-inertia factor of Mars | Q57862724 | ||
An improved solution of the gravity field of Mars (GMM-2B) from Mars Global Surveyor | Q58091022 | ||
Electrical conductivity of the Earth's lower mantle | Q59068123 | ||
A new seismic velocity model for the Moon from a Monte Carlo inversion of the Apollo lunar seismic data | Q59664539 | ||
Crustal magnetic field of Mars | Q59759199 | ||
Inferring upper-mantle temperatures from seismic velocities | Q59789189 | ||
Mars gravity field: Combined Viking and Mariner 9 results | Q59938521 | ||
The interior structure of Mars: Implications from SNC meteorites | Q59938553 | ||
Thickness of the Martian crust: Improved constraints from geoid-to-topography ratios | Q59938555 | ||
Network science landers for Mars | Q60369519 | ||
The NetLander very broad band seismometer | Q60710594 | ||
Stability of majorite (Mg, Fe)SiO3 at high pressures and 1800°C | Q60722557 | ||
Constraints on seismic velocities in the Earth from traveltimes | Q63344509 | ||
Single-crystal elasticity of γ-(Mg0.91Fe0.09(2SiO4to high pressures and to high temperatures | Q63930538 | ||
Temperature derivatives of elastic moduli of (Mg0.91Fe0.09)2SiO4 modified spinel | Q63930543 | ||
Sound velocities and elastic properties of Fe-bearing wadsleyite and ringwoodite | Q63930557 | ||
Sensitivities of seismic velocities to temperature, pressure and composition in the lower mantle | Q63946671 | ||
Electrical conductivity of olivine, wadsleyite, and ringwoodite under upper-mantle conditions | Q95433323 | ||
Structure of the Moon | Q101074130 | ||
Thermal equation of state of magnesiowüstite (Mg0.6Fe0.4)O | Q107269627 | ||
Garnet–ilmenite–perovskite transitions in the system Mg4Si4O12–Mg3Al2Si3O12 at high pressures and high temperatures: phase equilibria, calorimetry and implications for mantle structure | Q107269633 | ||
Elasticity of Majorite and a Majorite-Pyrope solid solution to high pressure: Implications for the Transition Zone | Q107271071 | ||
An experimental investigation of the pyroxene-garnet transformation in a pyrolite composition and its bearing on the constitution of the mantle | Q107275004 | ||
Ultrahigh-pressure phase relations in the system Mg4Si4O12Mg3Al2Si3O12 | Q107275007 | ||
Single-crystal elasticity of pyrope and MgO to 20 GPa by Brillouin scattering in the diamond cell | Q107275324 | ||
Post-garnet transitions in the system Mg4Si4O12–Mg3Al2Si3O12 up to 28 GPa: phase relations of garnet, ilmenite and perovskite | Q107275327 | ||
P-V-T equation of state of MgSiO3 perovskite | Q107275340 | ||
Computation of seismic profiles from mineral physics: the importance of the non-olivine components for explaining the 660 km depth discontinuity | Q107275345 | ||
Calorimetric study on majorite–perovskite transition in the system Mg4Si4O12–Mg3Al2Si3O12: transition boundaries with positive pressure–temperature slopes | Q107275351 | ||
Theoretical seismic models of Mars: the importance of the iron content of the mantle | Q107275361 | ||
The electrical conductivity of the lower mantle phase magnesiowüstite at high temperatures and pressures | Q107275370 | ||
Laboratory-based electrical conductivity in the Earth's mantle | Q107275373 | ||
Evaluation of (Mg,Fe) partitioning between silicate perovskite and magnesiowustite up to 120 GPa and 2300 K | Q107275374 | ||
Mineralogy of the Martian interior up to core-mantle boundary pressures | Q107275435 | ||
Experimental Determination of the Electrical Conductivity of the Material of the Earth's Lower Mantle | Q107275464 | ||
Elasticity, composition and temperature of the Earth’s lower mantle: a reappraisal | Q107275488 | ||
P433 | issue | E4 | |
P407 | language of work or name | English | Q1860 |
P921 | main subject | aquatic science | Q4782809 |
P577 | publication date | 2005-01-01 | |
P1433 | published in | Journal of Geophysical Research | Q2738009 |
P1476 | title | Interior structure of terrestrial planets: Modeling Mars' mantle and its electromagnetic, geodetic, and seismic properties | |
P478 | volume | 110 |
Q107271030 | Constraining the composition and thermal state of Mars from inversion of geophysical data |
Q107271034 | Constraints on thermal state and composition of the Earth's lower mantle from electromagnetic impedances and seismic data |
Q57886708 | Geophysical constraints on the lunar Procellarum KREEP Terrane |
Q97885360 | Observations, Meteorites, and Models: A Preflight Assessment of the Composition and Formation of (16) Psyche |
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