The Ashele Cu polymetallic deposit in northern Xinjiang, which was formed in an active continental margin of SW Siberia in the late Paleozoic, is a marine volcanic massive sulfide deposit.

• 摘要新疆北部阿舍勒铜锌多金属矿床为海相火山岩型块状硫化物矿床，形成于晚古生代西伯利亚西南缘活动陆缘环境。