一个坑道周围的等温线可以理解为原始温度场的叠加。
The geoisotherms around a gallery can be explained as a superposition of the original temperature field.
三是包裹体后生变化（再平衡）的鉴别和原始温度的恢复。
The third problem was distinguishment of inclusion re equilibrium and recovery of primal temperature.
在附录中，我们还给出了重庆地区季节过渡日的大地原始温度图及各种材料的热传导率图。
The undisturbed ground temperature of the seasons' transitional days in Chongqing and the chart of some kinds of material's heat conductivities are given in the Appendix A and Appendix B .
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