It is a new attempt to study mineralization age using fission track method.
应用裂变径迹法研究成矿时代是一新的尝试。
Apatite fission track is a powerful tool to study the thermal history of sedimentary basin.
磷灰石裂变径迹是研究沉积盆地地热史的强有力工具。
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.
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。
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