Laboratory studies into the effect of regolith on planetary X-ray fluorescence spectroscopy
In the analysis of X-ray fluorescence spectra from planetary surfaces, it is traditionally assumed that the observed surface is a plane-parallel, smooth, and homogeneous medium. The spectral and spatial resolutions of the instruments that have been used to measure X-ray emission from planetary surfaces to date have been such that this has been a
Näränen, Jyri et al.
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2008