“…The first issue is the spatial distribution of the suture, for which there are three main viewpoints: 1) from northern Solonker via Xilinhot to Ulanhot (Xu and Chen, 1997;Xu et al, 2013), 2) from Solonker via Xilinhot to Horqinyouzhongqi (Li, 1987;Pan and Xiao, 2015;Fu et al, 2017) or via Sonidyouqi to Linxi (Wang and Liu, 1986;Xiao et al, 2003Xiao et al, ., 2009, 3) from southern Solonker to Xar-Moron River (Li, 2006;Jian et al, 2010;Liu et al, 2013;Pan and Xiao, 2015;Liu et al, 2017). Furthermore, the tectonic setting of the late Paleozoic magmatism, especially during the early Permian, is disputed, with conflicting interpretations such as: 1) continental arc or subduction setting (Miao et al, 2007;Tong et al, 2010;Liu J F et al, 2011Liu J F et al, , 2016Liu R et al, 2016), 2) post-orogenic extension setting (Li et al, 2012(Li et al, , 2014a, 3) intraplate rift or retro-arc basin setting Wang et al, 2014;Xu et al, 2014Xu et al, , 2018Song et al, 2015;Luo et al, 2016;Shao et al, 2017). In the present work, we present new zircon U-Pb ages, in-situ zircon Hf isotopes, whole-rock geochemistry and Sr-Nd isotopes for the early Permian intrusive rocks from Ar-Horqin, southeastern Inner Mongolia.…”