Comments |
Average grade of 0.07% Mo. Occurrence, large from Nokleberg and others (2006). Associated with granite-granodiorite and leucogranite intrusions. Gangue minerals are quartz, feldspar, sericite, and carbonate. Consists of a Cu-Mo stockwork hosted in Proterozoic schist and gneiss intruded by a Paleozoic granitoid stock. The host rocks are altered to K-feldspar, silica, and sericite. A hydrothermal alteration zone contains some intensely brecciated and silicified areas. |
Study area name |
Central Asian Orogenic Belt |
References |
Petrov and Mkrtychan (1976); Nokleberg and others (1999); Nokleberg and others (2003); Nokleberg and others (2006); Rundkvist (2001); Andrei F. Chitalin (written commun., 2009) |
Site reference |
Mihalasky, Ludington, Hammarstrom, and others (2015) |