“…For example, ore deposit formed in the Paleozoic is represented by Duobaoshan porphyry Cu-Mo deposit (475.9 ± 6.9 Ma, Zeng et al 2014), associated with the Paleozoic intrusions, and are considered to be related to the closure of the Paleo-Asian ocean; ore deposits formed in the Mesozoic are represented by Taipingchuan Cu-Mo deposit (203 Ma, Chen et al, 2010), Daheishan Mo deposit (168.2 ± 3.2 Wang et al, 2009), Tongshan Cu-Mo deposit (150.9 ± 0.8 Ma, H.J. Chen et al, 2011), and Chalukou Mo deposit (148 ± 1 Liu et al, 2014), associated with the Mesozoic intrusions (Liu et al, 2001;Mao et al, 2003;Zeng et al, 2010;Mao et al, 2011;Zeng et al, 2011), and are considered to be related to the subduction of the MongolOkhotsk Ocean and post-collisional extension (Zorin, 1999;Fan et al, 2003;Meng, 2003) or the subduction of the Paleo-Pacific Ocean (Hilde et al, 1977;F. Wang et al, 2006;Y.B.…”