about
Peak-ring structure and kinematics from a multi-disciplinary study of the Schrödinger impact basinStructure and evolution of the lunar Procellarum region as revealed by GRAIL gravity dataGRGM900C: A degree 900 lunar gravity model from GRAIL primary and extended mission data.Lunar bulk chemical composition: a post-Gravity Recovery and Interior Laboratory reassessment.Geochemical arguments for an Earth-like Moon-forming impactorLunar exploration: opening a window into the history and evolution of the inner Solar System.Formation of the Orientale lunar multiring basin.Heterogeneity in lunar anorthosite meteorites: implications for the lunar magma ocean modelDetection of the lunar body tide by the Lunar Orbiter Laser AltimeterThe formation of peak rings in large impact cratersLunar impact basins revealed by Gravity Recovery and Interior Laboratory measurementsAn asteroidal origin for water in the MoonIsotopes as tracers of the sources of the lunar material and processes of lunar origin.Gravity field of the Orientale basin from the Gravity Recovery and Interior Laboratory MissionContraction or expansion of the Moon's crust during magma ocean freezing?New approaches to the Moon's isotopic crisis.The tidal-rotational shape of the Moon and evidence for polar wander.Asymmetric distribution of lunar impact basins caused by variations in target properties.The origin of lunar mascon basinsGravity field of the Moon from the Gravity Recovery and Interior Laboratory (GRAIL) missionAncient igneous intrusions and early expansion of the Moon revealed by GRAIL gravity gradiometry.Evidence for a Low Bulk Crustal Density for Mars from Gravity and Topography.Primordial clays on Mars formed beneath a steam or supercritical atmosphere.Identification of buried lunar impact craters from GRAIL data and implications for the nearside mariaMineralogical Diversity and Geology of Humboldt Crater Derived Using Moon Mineralogy Mapper Data.Thickness of the crust of Mercury from geoid-to-topography ratiosOn the possibility of viscoelastic deformation of the large south polar craters and true polar wander on the asteroid VestaVolatile loss following cooling and accretion of the Moon revealed by chromium isotopesHow large are present-day heat flux variations across the surface of Mars?Thermal evolution and Urey ratio of MarsModelling of compaction in planetesimalsAsymmetric thermal evolution of the MoonEvidence of impact melt sheet differentiation of the lunar South Pole-Aitken basinFeatureless spectra on the Moon as evidence of residual lunar primordial crustGlobal occurrence trend of high-Ca pyroxene on lunar highlands and its implicationsVariation of the lunar highland surface roughness at baseline 0.15-100 km and the relationship to relative ageConvection-driven compaction as a possible origin of Enceladus's long wavelength topographyReflection imaging of the Moon's interior using deep-moonquake seismic interferometryThe effect of target properties on transient crater scaling for simple cratersThe fractured Moon: Production and saturation of porosity in the lunar highlands from impact cratering
P2860
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P2860
description
2012 nî lūn-bûn
@nan
2012年の論文
@ja
2012年論文
@yue
2012年論文
@zh-hant
2012年論文
@zh-hk
2012年論文
@zh-mo
2012年論文
@zh-tw
2012年论文
@wuu
2012年论文
@zh
2012年论文
@zh-cn
name
The crust of the Moon as seen by GRAIL.
@en
type
label
The crust of the Moon as seen by GRAIL.
@en
prefLabel
The crust of the Moon as seen by GRAIL.
@en
P2093
P2860
P50
P356
P1433
P1476
The crust of the Moon as seen by GRAIL
@en
P2093
Alexander S Konopliv
David E Smith
Francis Nimmo
Frank G Lemoine
G Jeffrey Taylor
H Jay Melosh
James G Williams
Jeffrey C Andrews-Hanna
Maria T Zuber
Michael M Watkins
P2860
P304
P356
10.1126/SCIENCE.1231530
P407
P577
2012-12-05T00:00:00Z