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Progress in Earth and Planetary Science
Fig. 3 | Progress in Earth and Planetary Science

Fig. 3

From: Formation, preservation and extinction of high-pressure minerals in meteorites: temperature effects in shock metamorphism and shock classification

Fig. 3

The shock temperatures of common rocks and meteorites, calculated by the Hugoniot integral approximation, using the parameters in Table 1. SMG is San Marcos gabbro. The representative solidus and liquidus of ultramafic/mafic rocks are for chondrites (OC) from Agee et al. (1995) and basalt (B) from Hirose et al. (1999) and Andrault et al. (2011)

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