“…Moreover, the postpeak curves present two different failure characteristics (Figure 3). One shows an apparent brittle failure characteristic (such as granite, diorite, quartzite, limestone, gneiss, dolomite, shale, metamorphic sandstone, and quartz schist), and the other shows an obvious ductile failure characteristic (such as mudstone, physicochemical slate, schist, porphyrite, sandstone, and marble) [29,30].…”