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.
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