裂变径迹分析显示样品应处于剥露的部分退火带，其表观年龄主体表现为冷却年龄，部分具混合年龄特征。
The fission track analyses show that these samples are under the exhumed partial annealing zone and the apparent ages obtained are cooling ages with part mixed ages.
通过对鄂尔多斯盆地磷灰石裂变径迹资料深入分析与反演模拟，定性-半定量地研究了该区相关岩石组合的地热演化史。
By analyzing apatite fission track data and inverse modeling, the thermal history of relevant rock assemblage has been studied qualitatively to semi-quantitatively in Ordos basin.
通过磷灰石裂变径迹热史模拟的方法，精确揭示了在新生代时期松辽盆地与大兴安岭的热构造史，并分析了它们的盆山耦合关系。
Thermal history simulation of Apatite Fission Track shows that the thermal structure history in Cenozoic and the relationship between Songliao Basin and Dahinganling Mountain.
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