Comments |
Partial resource of 27.4 Mt at 0.46% Cu. Could be a massive sulfide deposit. Copper sulfide minerals in shear zones in a dacite porphyry that intrudes pyroclastic rocks. A weak zone of secondary enrichment is 13 m thick and consists of bornite, chalcocite, and covellite. Associated with bimodal (basalt-rhyolite) assemblage rocks. Nokleberg (2010) classifies it as a porphyry, while Petrov and others (2009) indicates it is a volcanic massive sulfide. |
Study area name |
Central Asian Orogenic Belt |
References |
Andrei F. Chitalin (written commun., 2009); Lapukhov (1975); Kuznetsov (1982); Nokleberg and others (1999); Nokleberg and others (2003); Nokleberg and others (2006); Nokleberg (2010); Rundkvist (2001); Petrov and others (2009) |
Site reference |
Mihalasky, Ludington, Hammarstrom, and others (2015) |