Astrobiological applications of μ-mapping X-ray fluorescence spectrometry

In situ elemental imaging of planetary surface regolith at a spatial resolution of 100s to 1000s of microns can provide evidence of the provenance of rocks or sediments and their habitability, and can identify post-depositional diagenetic alteration affecting preservation. We use high-resolution ele...

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Bibliographic Details
Published inInternational journal of astrobiology Vol. 23
Main Authors Blake, David Frederick, Walroth, Richard C., Bristow, Thomas F., Sarrazin, Philippe, Gailhanou, Marc, Thompson, Kathleen, Downs, Robert Terrance, Yen, Albert Shi-Yuen, Marchis, Franck, Webb, Samuel, Chalumeau, Clement, Solé, Vincente Armando, Walter, Philippe, Chen, Jianxin, Henderson, Roger, Lafuente, Barbara
Format Journal Article
LanguageEnglish
Published Cambridge, UK Cambridge University Press 01.01.2024
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Summary:In situ elemental imaging of planetary surface regolith at a spatial resolution of 100s to 1000s of microns can provide evidence of the provenance of rocks or sediments and their habitability, and can identify post-depositional diagenetic alteration affecting preservation. We use high-resolution elemental maps and XRF spectra from MapX, a flight prototype in situ X-ray imaging instrument, to demonstrate this technology in rock types relevant to astrobiology. Examples are given for various petrologies and depositional/diagenetic environments, including ultramafic/mafic rocks, serpentinites, hydrothermal carbonates, evaporites, stromatolitic cherts and diagenetic concretions.
ISSN:1473-5504
1475-3006
DOI:10.1017/S147355042400003X