A lunar feldspathic breccia meteorite,
the Northwest Africa (NWA)
11273, was analyzed to compensate the lack of scientific data available
about its mineralogy and geochemistry. In order to obtain a deeper
characterization of the sample, a strategy based on the combination
of nondestructive spectroscopic techniques such as X-ray fluorescence
and Raman spectroscopy is used. Both techniques are being used in
spatial missions by the Perseverance Rover, so their combination in
the laboratory is here proposed as an optimal strategy to study the
complete mineralogy of the sample. In addition to finding the minerals
indicated by the Meteoritical Society (anorthite, olivine, pyroxene,
kamacite, and troilite), other minor minerals were identified, such
as zircon and ilmenite, which are minerals related to the Moon geology,
as well as calcite and sulfate which can be considered products of
terrestrial weathering. Finally, secondary minerals related to alteration
processes were also found, such as hematite, quartz, and anatase.
In this work, the alteration processes that gave rise to the detected
secondary minerals have been proposed.