“…Metasedimentary granulite enclaves are abundant in the Indo-Sinian peraluminous granites from the DSGB. In recent years, many papers have been published discussing the origin of these granites (e.g., Charoy and Barbey, 2008;Chen et al, 1995Chen et al, , 2011Deng, 2003;Deng et al, 2004;Fang, 1989;Hsieh et al, 2008;Peng et al, 2004;Qi et al, 2007;Zhao et al, 2010Zhao et al, , 2011, and their hosting granulite enclaves (e.g., Du et al, 1999;Pang, 2001;Peng, 2006;Peng et al, 2004;Wang, 1987;Zhao et al, 2010Zhao et al, , 2011. Two possible tectonic settings of the granitic magmatism have been proposed: (1) anatexic products formed during continental collision (e.g., Chen et al, 1995Chen et al, , 2011Deng, 2003;Deng et al, 2004;Fang, 1989;Hsieh et al, 2008;Qi et al, 2007); and (2) crustal melts of post-collisional extension (e.g., Charoy and Barbey, 2008;Peng et al, 2004;Zhao et al, 2010Zhao et al, , 2011.…”