“…Nitsan, 1977;Gomshei and Templeton, 1989). However, at laboratory scale, the generation of EMR was observed during deformation experiments on different materials, such as ice (Fifolt et al, 1993;, metals (Misra and Kumar, 2004), amorphous materials like glass ceramics (Bahat et al, 2002), and different rock types (Yamada et al, 1989;Enomoto and Hashimoto, 1992;Koktavy et al, 2004;Mori and Obata, 2008), mostly independent of their water saturation (Yoshida and Ogawa, 2004). These observations strongly restrict possible source mechanisms.…”