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依据野外地质调查和室内分析测试结果,对长江某坝址结晶岩中F_(54)泥化带进行了分析研究,认为其形成受控于断裂构造及水文地球化学作用,并伴随有元素的迁移和富集。
According to the results of field geological survey and laboratory analysis, the F 54 clay belt in the crystallization rock of a dam site in the Yangtze River has been analyzed. It is believed that its formation is controlled by faulting and hydrogeochemistry and accompanied by the migration of elements And enriched.