The Characteristics of Tectonic-Alteration and Mineralization at Wushan Copper Deposit, Jiangxi and Prognosis of Deep-Seated Ore Bodies

• 责任者：Li Ying (School of the Earth Sciences and Resources ; China University of Geosciences ; Beijing 100083 ; China) ; Lü Guxian
• 刊名：Contributions to Geology and Mineral Resources Research
• 出版年：2010
• 卷期：25(1)
• 关键词：铜矿 ; copper ores ; 江西 ; Jiangxi Province
• 页码：p.18-23
• 图表：4 illus，6 refs.
• 分类号：1001
• issnNo：ISSN1001-1412
• isbnNo：CN12-1131/P

///Wushan copper deposit is situated at the center of Jiujiang-Ruichang tectonic belt on the southern side of Yangtze river fracture and on the northern limb of Henglishan-Huangqiao syncline. Ore bodies occur at the uncoformity plane and the contact zones of Wushan intrusive body. The interformational fractural zones between the conglomeratic quartzite of Wutong formation of Upper Devonian Series and the dolomitic limestone of Huanglong formation of Middle Carboniferous Series and between Huanglong formation of Middle Carboniferous Series and limestone of Qixia stage of Lower Permian Series control the enrichment of massive polymetallic sulfide and formation of the ore bodies. Contact zones between Wushan intrusive body and limestone of Carboniferous System and Permian System and xenoliths control skarn ore bodies.