THE WALL ROCK ALTERATION AND ITS GEOCHEMICAL CHARACTERISTICS OF THE SHAZHOU DEPOSIT IN XIANGSHAN URANIUM ORE-FIELD
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摘要: 江西相山铀矿田沙洲铀矿床的矿体严格受断裂控制,围岩蚀变分带非常明显。对沙洲铀矿床围岩蚀变的地球化学特征进行的研究表明,沙洲矿床从矿石到围岩的化学成分具有明显的变化,这些化学成分的变化与蚀变过程中物质的带入带出是密切相关的。通过对全部样品进行R型聚类分析,确定矿床成矿元素组合为U、W、HREE、Th、Zn、Zr、Mo、Pb,这些元素可作为铀成矿预测标志。研究成果在一定程度上充实和丰富了沙洲铀矿床的成因认识。Abstract: The ore body of Shazhou deposit in Jiangxi Province is strictly controlled by faults and its wall rock alteration zoning characteristics is very apparent. This paper introduces the geochemical characteristics of the wall rock alteration. The results of whole-rock analysis of Shazhou deposit show that the chemical composition of the ore body is very different from the surrounding rock and the differences are relevant with the migration of chemical elements in the course of alteration. The combinations of metallogenetic elements are U, W, HREE, Th, Zn, Zr, Mo, Pb based on R-mode cluster analysis of all the rock samples and these elements can serve as the criteria for U ore prospecting in the region.
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图 1 相山铀矿田区域地质与铀矿床分布图[7]
1—白垩系砂砾岩;2—上侏罗统中酸性火山岩;3—次花岗斑岩;4—燕山期花岗岩;5—华力西期花岗岩;6—加里东期花岗岩;7—铀矿床;8—上三叠统砂岩;9—中元古界变质岩;10—远古宇(未分)变质岩;11—断裂;12—推测深大断裂;13—火山颈(推测);14—研究区
Figure 1. The regional geology and uranium deposit distribution of the Xiangshan ore-field
图 2 沙洲矿床地质构造与矿化示意图[3]
1—凝灰岩及流纹英安岩;2—碎斑熔岩;3—推覆体变质岩;4—基底变质岩;5—花岗岩;6—断裂构造;7—火山环状断裂;8—钻孔见矿范围;9—矿体
Figure 2. A map showing the geological structure and mineralization of Shazhou deposit
表 1 沙洲矿床-8 m、-58 m和-98 m中段矿体剖面主量元素化学成分
Table 1. Chemical compositions of the major elements from -8 m, -58 m and -98 m sections of Shazhou deposit
表 2 沙洲矿床-8 m、-58 m和-98 m中段矿体剖面微量元素含量(10-6)
Table 2. Chemical compositions of the trace elements from -8 m, -58 m and -98 m sections of Shazhou deposit
表 3 沙洲矿床-8 m、-58 m和-98 m中段矿体剖面稀土元素化学成分
Table 3. Chemical compositions of the rare-earth elements from -8 m, -58 m and -98 m sections of the Shazhou deposit
表 4 沙洲矿床岩石元素含量相关性分析矩阵
Table 4. Corellation matrix of the elements in rocks from Shazhou deposit
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