利用放射性同位素地质年代学和扩散年代测定法来追踪岩浆系统的热演化。
Leveraging radioisotope geochronology and diffusion chronometry to trace the thermal evolution of magmatic systems.
作者信息
Li Wei-Ran, Costa Fidel
机构信息
VRock Laboratory, Department of Earth Sciences, The University of Hong Kong, China.
NWU-HKU Joint Centre of Earth and Planetary Sciences, Department of Earth Sciences, The University of Hong Kong, China.
出版信息
Natl Sci Rev. 2025 Apr 11;12(9):nwaf141. doi: 10.1093/nsr/nwaf141. eCollection 2025 Sep.
Time scales determined by radioisotope geochronology and diffusion chronometry for the same magmatic systems have shown variable degrees of discrepancy. We show in this paper that this could be due to the different temperature ranges that the two types of chronometers are effectively sampling, therefore combining them will help to trace the thermal evolution of magmatic systems on Earth and other planets.
通过放射性同位素地质年代学和扩散年代学确定的同一岩浆系统的时间尺度显示出不同程度的差异。我们在本文中表明，这可能是由于这两种年代测定仪实际采样的温度范围不同，因此将它们结合起来将有助于追踪地球和其他行星上岩浆系统的热演化。
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