NanoSIMS O isotopic analysis of dolomite grains in the Angular Stone of Interest sample OREX-800055-17
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Description
The angular lithology SoI contains multiple forms of dolomite grains, including large grains, dispersed small isolated grains and dolomite-rich lozenge shaped regions. Some of the grains show complex internal structure revealed by cathodeluminesence. O-isotope measurements by NanoSIMS will provide insight into the relationship between the fluids associated with hte alteration events that createdt hese dolomites.
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How To Cite
Franchi, I., 2026. NanoSIMS O isotopic analysis of dolomite grains in the Angular Stone of Interest sample OREX-800055-17, Version 1.0. Astromaterials Data Archive. https://doi.org/10.60707/3qem-7717 Accessed 2026-05-11.
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Funding Sources
This material is supported by NASA under contract NNM10AA11C issued through the New Frontiers program. Analyses were funded by STFC Grant UKRI1026.
