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- Fission track thermochronologic constraints on plateau surface and geomorphic relief formation in the northwestern margin of the Tibetan Plateau 青藏高原西北缘高原面与陡坡地貌形成过程的裂变径迹热年代学约束
- Apatite fission track can be used as the index of thermal history inversion. 磷灰石裂变径迹可以作为反演热史的指标。
- The author points out some questions about using AFTA to study uplift rate and recommends the fission track length analysis should be emphasesed. 并分析了利用磷灰石裂变径迹研究隆升速率应当注意的问题，强调了加强径迹长度分析的研究
- Apatite fission track data suggest that the early Cretaceous strata in the Liupanshan basin were subjected to two burial heating events. 磷灰石裂变径迹研究表明，六盘山盆地白垩系地层经历两次埋深加热事件。
- Apatite fission track analysis was carried out to study the thermal evolution and timing of hydrogen generation in the Huahai Basin. 利用裂变径迹分析方法测量了取自花海拗陷的钻井磷灰石样品的裂变径迹年龄和长度。
- Thermal and denudational history of granitoid batholith recorded by apatite fission track in the Dulong River region in northwestern Yunnan,since Late Miocene. 滇西北独龙江岩体晚中新世以来的热史和剥蚀历史的磷灰石裂变径迹记录
- With the acquisition of the data of geodetic leveling, GPS and fission track, the uplift rates of the Qinghai-Tibet plateau (QTP) have been generalized. 笔者对近年在高原进行的大地水准测量、GPS、同位素年代学(~(39)Ar/~(40)Ar,裂变径迹等)结果进行了分析研究,扼要地阐述了青藏高原隆升过程和速率;
- Zheng Dewen, Zhang Peizhen, Wan Jinglin et.al. Apatite fission track evidence for thermal history of Liupanshan basin. Chinese Journal of Geoghysics, 2005, (1). 郑德文，张培震，万景林等。六盘山盆地热历史的裂变径迹证据。地球物理学报，2005年1期.
- The fission track data also indicate that the southern part of the batholith was affected by the collision event earlier than the middle and northern parts. 裂变径迹资料还揭示印藏碰撞先影响南部岩体，随后才波及到岩基中北段.
- Fluid inclusion microthermometry and apatite fission track analysis were used to reconstruct the Tertiary paleotemperature of the East depression,Liaohe basin. 以太阳岛构造和大平房构造为例,利用流体包裹体显微测温和磷灰石裂变径迹分析方法恢复了辽河盆地东部凹陷第三系的古地温。
- This paper introduced the inversion model of nolinear heatflow through the relation betweentheareal track number density of apatite fission track versus time and temperature. 本文应用磷灰石裂变径迹的面积径迹数随时间、温度变化的规律，建立非线性热流的反演模型。
- The lengths of confined fission track were used as a geothermometer to analyze the thermal history of each of the four single well and the erosion thickness of Dongying formation. 研究表明，热流演化随地质历史的发展是逐渐减小的，但在凹陷的不同部位减小的程度不同；
- Through the restoration of Wuzhishan tectonic history and analysis of apatite fission track, Wuzhishan structure was buildup at Himalayan movement stage has been shown. 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。
- The results showed that the fission track ages of quartz vary over a wide range from 1 Ma to 25 Ma in the four profiles, significantly younger than the ages of Triassic and Cambrian parent rocks. 结果显示:石英的裂变径迹年龄数据呈现出较大的变化范围,从1Ma到25Ma,且远远地小于其三叠纪和寒武纪的母岩年龄;
- There are two levels planation surfaces and one piedmont and several terraces.Secondly, The formation age of these leveled landforms is contrained by paleomagnetism, fission track dating. 通过沉积地层学、磁性地层、地层对比等多种研究方法限定了这些地貌面的形成时代；
- Yuan, Jennwei Huang, S.-T. and Liu, T.-K. (1987) Fission track dating of zircons in the late Cenozoic sedimentary rock in the Miaoli area, Taiwan. Petroleum Geology of Taiwan, 23, 41-53. 原振维、黄旭灿、刘聪桂(1987)苗栗地区新生代晚期沈积岩中锆石之核飞迹定年。台湾石油地质，第23号，第41-53页。
- The detrital apatite fission track ages of from the High No.3 far away from the Altyn Mountain indicate that there are two periods of uplifting and exhumation in the Altyn Mountains in Cretaceous. 而离阿尔金断裂稍远一些的三高点剖面样品的单颗粒AFT年龄反映了源区阿尔金山在白垩纪和古近纪存在两期隆升剥蚀。
- The thermal history of the Well TZ10 was simulated using vitrinite reflectance data and the new model.The thermal wave model was tested and verified by the apatite fission track data in the well. 利用该模型并结合镜质体反射率古温标模拟计算了塔中10井的热历史，同时用磷灰石裂变径迹数据对模拟结果进行了检验。
- Our pilotless rocket enters the track of the earth. 我们把一个无人驾驶的火箭送入了地球的轨道里。
- A NEW COUNTING METHOD FOR FISSION TRACK DENSITY 一种裂变径迹密度统计的新方法
