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ReportsThe Evolution of Mercurys Crust: A Global Perspective from MESSENGER
Mapping the distribution and extent of major terrain types on a planets surface helps to constrain the origin and evolution of its crust. Together, MESSENGER and Mariner 10 observations of Mercury now provide a near-global look at the planet, revealing lateral and vertical heterogeneities in the color and thus composition of Mercurys crust. Smooth plains cover approximately 40% of the surface, and evidence for the volcanic origin of large expanses of plains suggests that a substantial portion of the crust originated volcanically. A low-reflectance, relatively blue component affects at least 15% of the surface and is concentrated in crater and basin ejecta. Its spectral characteristics and likely origin at depth are consistent with its apparent excavation from a lower crust or upper mantle enriched in iron- and titanium-bearing oxides.
1 School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85251, USA.
2 Department of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, DC 20015, USA. 3 Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, USA. 4 National Museum of Natural History, Smithsonian Institution, Washington, DC 20560, USA. 5 Department of Geological Sciences, Brown University, Providence, RI 02912, USA. 6 Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institution, Washington, DC 20560, USA. * To whom correspondence should be addressed. E-mail: bdenevi{at}ser.asu.edu
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Science. ISSN 0036-8075 (print), 1095-9203 (online)