Post-hydration thermal metamorphism of carbonaceous chondrites

By Tomoki Nakamura. 2005

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Spectral reflectance properties of carbonaceous chondrites: 1. CI chondrites (2012, unknown): “…estimates for these thermally metamorphosed chondrites range from 600 to 900 C for B-7904, 700–850 C for Y-86720, and >700 C for Y-86789 (Akai, 1990, 1992, 1994; Akai and Tari, 1997; Lipschutz et al., 1999; Tonui et al., 2002; Nakamura, 2005, 2006; Nakamura et al., 2006; Nakato et al., 2009).”
Petrographic, chemical and spectroscopic evidence for thermal metamorphism in carbonaceous chondrites I: CI and CM chondrites (2014, background): “Nakamura (2005) also found that the behavior of Cd was not completely predictable at low to moderate heating levels.”
Modal mineralogy of CI and CI-like chondrites by X-ray diffraction (2015, methodology): “Subsequently, Y-82162 and Y-86029 have been classiﬁed as CI-like chondrites that experienced both extensive aqueous alteration and at least one post-hydration heating event (Ikeda, 1992; Tonui et al., 2003, 2014; Nakamura, 2005).”