华南花岗岩型铀矿的成因模式、数学模型和断裂成矿潜力估计法
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P619.140.1


THE METALLOGENETIC MODEL AND MATHEMATICAL MODEL FOR GRANITE-TYPE URANIUM DEPOSITS IN SOUTH CHINA AND THE EVALUATION METHOD FOR URANIUM ORE-FORMING POTENTIALITY IN FAULTS
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    摘要:

    本文基于对华南花岗岩型铀矿的成因模式和数学模型分析,提出了一种适用于华南花岗岩区各级序成矿断裂铀资源评价的方法-断裂成矿潜力估计法。这种方法,因把工作重点放在断裂上,它具有工作量少而收效好的优点。文中列举的实例表明,在华南花岗岩区用该方法作铀资源评价,效果优于其他方法。

    Abstract:

    This paper deals with an advance in a new method applicable to the evalua-tion of uranium resources in ore--forming faults of different orders in granite areasof South China--The evaluation method for uranium ore--forming potentiality infaults, which is based on the metallogenetic model and mathematical model ofgranite-type uranium deposits in South China. Since the emphasis of the methodis placed on faults, it has the advantages of doing less work and yielding goodresults. The example in the paper indicates clearly that this method used inevaluating uranium resources in granite areas of South China can yield betterresults than other methods.

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李明连.1992.华南花岗岩型铀矿的成因模式、数学模型和断裂成矿潜力估计法[J].地质论评,38(1):75-81,[DOI].
Li Minglian Institute, South China Bureau of Geological Exploration, Ministry of Nuclear Industry, Shaoguan, Guangdong.1992. THE METALLOGENETIC MODEL AND MATHEMATICAL MODEL FOR GRANITE-TYPE URANIUM DEPOSITS IN SOUTH CHINA AND THE EVALUATION METHOD FOR URANIUM ORE-FORMING POTENTIALITY IN FAULTS[J]. Geological Review,38(1):75-81.

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