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Characterising the CI and CI like carbonaceous chondrites using thermogravimetric analysis and infrared spectroscopy

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Figure

Figure 1 shows the DTG (wt.%/°C) curves for thephyllosilicate, Fe-(oxy)hydroxide and carbonate stand-ard minerals
Fig. 2 Mass loss and DTG curves for CI chondrites Ivuna and Orgueil, and CI-like Y-82162 and Y-980115
Table 1 Mass loss (wt.%) as a function of temperature for the CI and CI-like chondrites.
Fig. 3 Mid-IR spectra for CI chondrites Ivuna and Orgueil, and CI-like Y-82162 and Y-980115
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