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本文从元素迁移和同位素交换出发，研究崇浦地区粒状碎斑熔岩和５７０铀矿区熔结状流纹岩的水─岩氧同位素相互作用，并用缓冲开放系统模式估计水─岩氧同位素相互作用的持续时间。
Based on element migration and isotope exchange, the water-rock oxygen isotope interaction between grained crushed lavas in the Chongpu area and the fused rhyolite in the 570 uranium ore area was studied. The water-rock oxygen isotope interaction between the water-rock oxygen isotopes duration.