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Digital Topography Models for Martian Surfaces

IEEE Geoscience and Remote Sensing Letters, 2005
We propose to use an unsupervised automated classification of topographic features on Mars in order to speed up geomorphic and geologic mapping of the planet. We construct a digital topography model (DTM), a multilayer grid that stores various kinds of topographical information for every pixel in a site.
Tomasz F. Stepinski, Ricardo Vilalta
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Martian surface and crust: Review and synthesis

Icarus, 1973
The nature of the classical marking of Mars are studied on the basis of Mariner 9 data and some earlier data. The analysis leads to a model of the Martian crust. Evidence for petrologic distinctions between surface materials in dark and light regions is obtained.
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Dielectric Map of the Martian Surface

2005
We have undertaken laboratory electromagnetic characterization of the total set of minerals identified by TES [1] on the Martian surface in order to investigate experimentally the dielectric properties of the sediments covering it in the frequency range from 1 to 1000 MHz.
Heggy, Essam, Pommerol, Antoine
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pH of the Martian surface

Planetary and Space Science, 1995
Allan A. Mills, Mark R. Sims
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The Martian Surface

2008
Phenomenal new observations from Earth-based telescopes and Mars-based orbiters, landers, and rovers have dramatically advanced our understanding of the past environments on Mars. These include the first global-scale infrared and reflectance spectroscopic maps of the surface, leading to the discovery of key minerals indicative of specific past climate ...
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Some comments on “the composition of the Martian surface”

Icarus, 1965
Martian surface composition of either fine or coarse grained silicates coated with finely divided ...
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Polarimetric and photometric simulation of the Martian surface

Icarus, 1969
Abstract An approach is presented to obtain a truly rational interpretation of the Martian surface and atmosphere. Polarimetric and photometric properties of ore specimens (limonite, siderite, desert varnish, and serpentine), considered good prospects for the Martian surface, are presented for the colors B(0.48 μ), G(0.54 μ), and I(1.0 μ).
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Surface processes modifying Martian craters

Icarus, 1968
Abstract Martian craters, even through many times more abundant than thought from initial inspection of Mariner IV photos, are less numerous, shallower, and have gentler slopes than craters on lunar uplands. This implies more effective action on Mars of some exogenous process or processes of erosion or deposition.
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Antibody–drug conjugates: Smart chemotherapy delivery across tumor histologies

Ca-A Cancer Journal for Clinicians, 2022
Javier Cortés   +2 more
exaly  

Surface Pressures in the Martian Highlands and Lowlands

Nature, 1967
CONFLICTING opinions have been expressed on the question of elevation of the Martian dark areas (maria) relative to the bright areas (deserts).
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