Abstract
Reflectance spectra in the 1- to 2.5-micrometer wavelength region
of the surface of Europa obtained by Galileo's Near Infrared Mapping
Spectrometer exhibit distorted water absorption bands that indicate
the presence of hydrated minerals, The laboratory spectra of hydrated
salt minerals such as magnesium sulfates and sodium carbonates and
mixtures of these minerals provide a close match to the Europa spectra.
The distorted bands are only observed in the optically darker areas
of Europa, including the lineaments, and may represent evaporite
deposits formed by water, rich in dissolved salts, reaching the surface
from a water-rich layer underlying an ice crust.
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