The Qunjisayi intermediate-basic intruded subvolcanic complex is located in the Awulale Mountain of the western Tianshan, Xinjiang, and was formed in the rift structure environment after the collision orogenesis of the Late Palaeozoic Era.
新疆西天山的群吉萨依中基性侵入-次火山杂岩体,形成于晚古生代晚期后碰撞造山的裂谷构造环境。