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Lunar highlands are plagioclase-rich terrains produced by crystal floating in a Magma Ocean system. Lunar samples revealed the presence of anorthositic (plagioclase &gt; 90%) samples from the Highlands, associated to more mafic rocks. Recently, remote sensing data permit mapping those terrains with high spatial and spectral resolution allowing detection of plagioclase and mafic crystal field (C.F.) absorptions.

american mineralogist

The Second Conference on the Lunar Highlands Crust and New Directions. VNIR spectral variability of the igneous stratified Stillwater Complex: A tool to map lunar highlands