Title

Composition of Surface Materials on the Moons of Mars

Authors

Authors

C. M. Pieters; S. Murchie; N. Thomas;D. Britt

Comments

Authors: contact us about adding a copy of your work at STARS@ucf.edu

Abbreviated Journal Title

Planet Space Sci.

Keywords

Asteroid capture; Space weathering; Regolith; Phobos; Deimos; ITOKAWA DUST PARTICLES; SOLAR-SYSTEM; PHOBOS; DEIMOS; HETEROGENEITY; SPECTROSCOPY; METEORITE; FEATURES; VESTA; Astronomy & Astrophysics

Abstract

The two small asteroid-like bodies orbiting Mars, Phobos and Deimos, are low albedo and exhibit similar visible to near-infrared spectra. Determining the origin of these moons is closely tied to determining their composition. From available spectroscopic data Phobos exhibits two distinct types of materials across its surface, and data from both Mars Express and Mars Reconnaissance Orbiter have provided additional details about the properties of these materials and their spatial relation to one another. Although no prominent diagnostic absorptions have been detected, systematic weak features are seen in some data. An extensive regolith is observed to have developed on both moons with characteristics that may be unique due to their special environment in Mars orbit. Understanding the character and evolution of the regolith of Phobos and Deimos is central to interpreting the moons' physical and optical properties. The cumulative data available for compositional analyses across the surface of Phobos and Deimos, however, remain incomplete in scope and character and ambiguous in interpretation. Consequently the composition of the moons of Mars remains uncertain. (C) 2014 Elsevier Ltd. All rights reserved.

Journal Title

Planetary and Space Science

Volume

102

Publication Date

1-1-2014

Document Type

Article

Language

English

First Page

144

Last Page

151

WOS Identifier

WOS:000343838800013

ISSN

0032-0633

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