通过对五指山邻区构造史恢复和磷灰石裂变径迹分析，指出五指山构造形成于喜山期。
Through the restoration of Wuzhishan tectonic history and analysis of apatite fission track, Wuzhishan structure was buildup at Himalayan movement stage has been shown.
利用裂变径迹分析技术，并结合地质学研究方法，对库车坳陷晚白垩世隆升过程进行了研究。
The Late-Cretaceous uplifting process of the Kuqa Depression was investigated using the fission track (FT) technique and the geological analysis. The uplifting has occurred for about 89 million years.
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.
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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