论文部分内容阅读
含有固体核径迹的地质样品在热退火时能够放出显著的热量,释放的热量与所含的固体核径迹的密度密切相关,通过用热分析法测量地质样品中所含的固体核径迹沉积的能量可以研究地质年代和地质热历史。
Geological samples containing solid nuclear track can emit significant heat during thermal annealing. The heat released is closely related to the density of solid nuclear track contained. By using thermal analysis to measure the solid nuclear track contained in the geological sample Deposited energy can study geologic age and geological thermal history.