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Copyright © 2014 by The Geochemical Society of Japan. tential for further exploration because of its location in the Jinshajiang tectonic zone (Pan et al., 2001). Previous studies have focused on the stratigraphic schemes for the Yangla region (He et al., 1998; Qu et al., 2004; Zhu et al., 2009a), type of deposits present (Lu et al., 1999; Wei et al., 2000), geochemistry of the Yangla granite (Wei et al., 1997, 2000), and geochronology of the Yangla granite (Wang et al., 2010). Though the systematic study of the source of the ore-forming materials of the deposit is of great significance, it has not yet been conducted. To Isotope geochemistry and its implications in the origin of Yangla copper deposit, western Yunnan, China