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利用径迹相交法研究了经部分退火后橄榄石中重离子径迹的显示问题。实验发现,对于给定的离子和退火条件,平均体径迹长度有很大的分散,其原因很可能与径迹相对于晶体的取向有关。
The trace of heavy ions in olivine after partial annealing was studied by using the track intersection method. It has been found experimentally that for a given ion and annealing conditions, the average body track length is greatly dispersed, probably due to the track orientation relative to the crystal.