图13 东海县南地温测量结果和推测热岩石圈深度与温度。
Fig. 13 Geothermal measurements and inferred lithospheric depth and temperature.
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.
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.
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