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<dc:title>ExoMars Raman Laser Spectrometer (RLS): development of chemometric tools to classify ultramafic igneous rocks on Mars</dc:title>
<dc:creator>Veneranda ., Marco</dc:creator>
<dc:creator>López Reyes, Guillermo Eduardo</dc:creator>
<dc:creator>Manrique Martínez, José Antonio</dc:creator>
<dc:creator>Sanz Arranz, José Aurelio</dc:creator>
<dc:creator>Lalla, Emmanuel Alexis</dc:creator>
<dc:creator>Konstantinidis, Menelaos</dc:creator>
<dc:creator>Moral Inza, Andoni Gaizka</dc:creator>
<dc:creator>Medina García, Jesús</dc:creator>
<dc:creator>Rull Pérez, Fernando</dc:creator>
<dc:subject>Espectroscopia Raman, Quimiometría, Marte, Rocas</dc:subject>
<dc:description>Producción Científica</dc:description>
<dc:description>This work aims to evaluate whether the multi-point analysis the ExoMars Raman Laser Spectrometer &#xd;
(RLS) will perform on powdered samples could serve to classify ultramafc rocks on Mars. To do &#xd;
so, the RLS ExoMars Simulator was used to study terrestrial analogues of Martian peridotites and &#xd;
pyroxenites by applying the operational constraints of the Raman spectrometer onboard the Rosalind &#xd;
Franklin rover. Besides qualitative analysis, RLS-dedicated calibration curves have been built to &#xd;
estimate the relative content of olivine and pyroxenes in the samples. These semi-quantitative results, &#xd;
combined with a rough estimate of the concentration ratio between clino- and ortho-pyroxene &#xd;
mineral phases, were used to classify the terrestrial analogues. XRD data were fnally employed as &#xd;
reference to validate Raman results. As this preliminary work suggests, ultramafc rocks on Mars could &#xd;
be efectively classifed through the chemometric analysis of RLS data sets. After optimization, the &#xd;
proposed chemometric tools could be applied to the study of the volcanic geological areas detected &#xd;
at the ExoMars landing site (Oxia Planum), whose mineralogical composition and geological evolution &#xd;
have not been fully understood</dc:description>
<dc:date>2021-04-19T20:58:26Z</dc:date>
<dc:date>2021-04-19T20:58:26Z</dc:date>
<dc:date>2020</dc:date>
<dc:type>info:eu-repo/semantics/article</dc:type>
<dc:identifier>Scientifc Reports, Octubre 2020, vol. 10, n. 16954. p. 1-14</dc:identifier>
<dc:identifier>2045-2322</dc:identifier>
<dc:identifier>http://uvadoc.uva.es/handle/10324/46255</dc:identifier>
<dc:identifier>10.1038/s41598-020-73846-y</dc:identifier>
<dc:identifier>1</dc:identifier>
<dc:identifier>16954</dc:identifier>
<dc:identifier>14</dc:identifier>
<dc:identifier>Scientific Reports</dc:identifier>
<dc:identifier>10</dc:identifier>
<dc:identifier>2045-2322</dc:identifier>
<dc:language>eng</dc:language>
<dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
<dc:publisher>Nature Research</dc:publisher>
<dc:publisher>Nature Research</dc:publisher>
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