Host: Japan Association of Mineralogical Sciences
X-shaped Japan-law twins of quartz from two localities in Japan, i.e., Oshigahae, Miyazaki Prefecture and Mitsuiwa, Gunma Prefecture, were analyzed by cathodoluminescence and EBSD. It was revealed that all of the examined samples evolved from a single center and developed as penetration twins. This formation mechanism is in contrast to the previously believed mechanism, which considers the X-shaped twins as a result of a combination of two y-shaped twins.