Constraints on Mars' crustal structure from correlations of gravity and areoid with topography
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topography Mars aeroid gravity↗
Engineering topics
Kucinskas, A.
Publications and source records attributed to Kucinskas, A..
Constraints on Mars' crustal and lithospheric properties from Mars Global Surveyor data
We used comparisons of gravity and geoid with topography in the spatial and spectral domains, together with additional information from the geologic record, to constrain support mechanisms for loads on the surface of Mars and their implications for the planet's crustal and lithospheric properties and evolution.
Mars crustal↗
An Improved 360 Degree and Order Model of Venus Topography
We present an improved 360 degree and order spherical harmonic solution for Venus' topography. The new model uses the most recent set of Venus altimetry data with spacecraft positions derived from a recent high resolution gravity model.
Venus↗
Gravity Results from Lunar Prospector
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Gravity Luna Prospector Deep Space Network↗
Isostatic Compensation of Ishtar Terra
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Magellan Ishtar Terra isostatic compensation Venus↗
Isostasy Models and Correlations of Geoid and Topography Data for Characteristic Highlands on Venus
We have used the newest solution for the Venus geopotential, incorporating tracking data from the circularized orbit of Magellan, along with global Venus topography data to study correlations of geoid and topography variations in several regions characteristic of the principal classes of highlands found on Venus.
geoid and topography data isostatic compensation m↗
Isostatic Compensation of Equatorial Highlands on Venus
We have used spherical harmonic models for Venus' global topography and graviy incorporating data from the Magellan mission to test isostatic compensation models in several equatorial highlands.
global↗
Geoid and Topography Correlations Compared with Various Isostatic Compensation Models for the Equatorial Highlands of Venus
High resolution interpretations relating gravity and topography data for Venus should be restricted to the equatorial regions at this time.
isostatic geoid anomalies isostatic compensation m↗