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MicroRaman Spectroscopy of Carbonaceous Chondrites to Constrain Peak Metamorphic Temperature and Mineralogy

  • Authors: Lorraine Roselló Del Valle, Kerri L. Donaldson Hanna, Bertrand Chazallon, Cristian Fosca, Claire Pirim, Christopher Bennett

Lorraine Roselló Del Valle et al 2026 The Planetary Science Journal 7 .

  • Provider: AAS Journals

Caption: Figure 14.

Left: ΓD plotted as a function of ωD, with the full parameter space on top and the boxed-in region zoomed in on the bottom. Right: ΓG plotted as a function of ωG, with the full parameter space on top and the boxed-in region zoomed in on the bottom. In the top images, the marker color indicates the petrologic type of the sample: type 1 (blue), type 2 (green), or type 3 (red). In the bottom images, the marker color indicates the specific meteorite. Markers without borders are the mean values of the maps, and their error bars represent the 1σ standard deviations. Markers with a black border are the values obtained for the single-spot spectra, and their error bars represent the 1σ confidence bounds.

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