提出一种新的由矿物中封闭径迹长度分布求解地质热历史的反演模拟计算方法，由该方法可得到地质热历史的唯一解。
A new inverse method for geothermal history calculation has been suggested. Differing from other methods this one can give an unique solution.
提出一种新的由矿物中封闭径迹长度分布求解地质热历史的反演模拟计算方法，由该方法可得到地质热历史的唯一解。
A new inverse method for geothermal history calculation has been suggested. Differing from other methods this one can give an unique solution.
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