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海洋放射年代学,是以海洋为对象测定地质时间序列的同位素年代学的一门分支学科,也是海洋同位素地球化学的重要组成部分。应用放射核素随时间呈指数衰减的特性进行年龄测定;利用核素本身的放射性做示踪原子,研究其空
Marine radiochronology is a branch of isotope geochronology that determines the geologic time series based on the ocean and is also an important part of marine isotope geochemistry. The age of radionuclides is exponentially decayed over time. Using the radionuclide itself as a tracer atom,