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《Progress In Precambrian Research》 2002-Z1
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The Characteristics and Origin of Iron REE Poly-Metal Deposits Related to Rift System of Middle Proterozoic in the Western Part of Northern Margin of North China Block

CAO Xiu-lan(Tianjin Institute of Geology and Mineral Resources, Tianjin 300170)  
The large-scaled poly-metal deposits formed in Mesozoic in Langshan-Baiyunebo rift system occurred in western part of northern margin of North China Block are expected to be the significant suppliers of Iron, REE, Copper, Lead and Zinc ore resources in China.The formation of these poly-metal deposits, which are controlled by strata and structures obviously, are directly related to the rifting. They are hydrothermal solution sedimentation poly-metal deposits trapped in sedimentary rock series. The characteristics and origin of deposits occurred from inner branch to outer branch of Langshan-Baiyunebo rift system show a certain degree of difference because of the variation of geological environment and ore compositions. Baiyun'ebo Iron REE deposit is hydrothermal solution sedimentation deposit with high quantities of Potassium, Sodium and Phosphorus. Huogeqi Copper Lead Zinc deposit is belong to transitional hydrothermal solution sedimentation deposit influenced by medium-basic volcanism and Dongshengmiao and Jiashengpan Lead Zinc deposits are hydrothermal sedimentation poly-metal deposits. All these typical deposits have been studied and discussed respectively in this paper.
【Fund】: 中国地质调查局“华北地台成矿规律和找矿方向综合研究项目”(编号 :2 0 0 110 2 0 0 0 38)
【CateGory Index】: P618.2
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