Element migration of pyrites during ductile deformation of the Yuleken porphyry Cu deposit (NW-China)

Online link https://doi.org/10.1016/j.oregeorev.2017.10.019
Description The strongly deformed Yuleken porphyry Cu deposit (YPCD) occurs in the Kalaxiangar porphyry Cu belt (KPCB), which occupies the central area of the Central Asian Orogenic Belt (CAOB) between the Sawu’er island arc and the Altay Terrane in northern Xinjia
Originators Hong, Tao; Xu, Xing-Wang; Gao, Jun; Peters, Stephen; Li, Jilei; Cao, Mingjian; Xiang, Peng; Wu, Chu; and You, Jun
Publication Ore Geology Reviews