磷灰石裂变径迹是研究沉积盆地地热史的强有力工具。
Apatite fission track is a powerful tool to study the thermal history of sedimentary basin.
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 data suggest that the early Cretaceous strata in the Liupanshan basin were subjected to two burial heating events.
作者用磷灰石裂变径迹法研究了准噶尔盆地艾参1井和火南1井主要生油层的热历史。
The authors studied the thermal history of the main source beds of Aican-1and Huonan-1 Wells in Junggar Basin by apatite fission-track.
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