Fig. 1From: Formation, preservation and extinction of high-pressure minerals in meteorites: temperature effects in shock metamorphism and shock classificationPressure–volume Hugoniots of L chondrite from mineral mixing models (Schmitt et al. 1994; Xie et al. 2006b) and shock experiment (Anderson and Ahrens 1998) along with a calculated dense isentrope. ΔEV is the internal energy difference between the isentropic and Hugoniot state of the same specific volumeBack to article page