实验结果表明，测量古径迹投影长度是揭示古地温状况的一种有效而简单的方法。
The experimental results show that measuring fossil track projected lengths is more powerful to reveal palaeotemperature and is very simple.
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.
应用推荐