1. METALS DEPOSITSThe Keyinbulake Cu—Zn deposit is located in the Chonghuer basin at the southern Altaids in Xinjiang. Ore bodies mainly occur in the exocontact zones between the Early Permian gran让e and the Lower D...1. METALS DEPOSITSThe Keyinbulake Cu—Zn deposit is located in the Chonghuer basin at the southern Altaids in Xinjiang. Ore bodies mainly occur in the exocontact zones between the Early Permian gran让e and the Lower Devonian Kangbutiebao Formation sedimentary rocks? Two mineralization periods can be distinguished based on ore occurrences, which include the submarine volcanic sedimentary exhalation and the metamorphic hydrothermal superimposition.展开更多
基金National Natural Science Foundation of China(50664008)Key Natural Science Foundation of Yunnan Province(05E024M)Novel Foundation of Kunming Institute of Precious Metals(2002BY-01).
文摘1. METALS DEPOSITSThe Keyinbulake Cu—Zn deposit is located in the Chonghuer basin at the southern Altaids in Xinjiang. Ore bodies mainly occur in the exocontact zones between the Early Permian gran让e and the Lower Devonian Kangbutiebao Formation sedimentary rocks? Two mineralization periods can be distinguished based on ore occurrences, which include the submarine volcanic sedimentary exhalation and the metamorphic hydrothermal superimposition.