Occurs within Carboniferous volcanic rock in the Keramay arc area (see Tang, Wang, Wyman and others, 2010, fig. 1). Proximal to Late Carboniferous adakitic and high-Mg dioritegranodiorite porphyry plutons (A-type) and dikes known for CuAu mineralization in the Baogutu area of the western Junggar region (see Tang, Wang, Wyman and others, 2010, fig. 1).
Study area name
Central Asian Orogenic Belt
Tang, Wang, Wyman and others (2010)
Mihalasky, Ludington, Hammarstrom, and others (2015)