有关地热条件的所有实验研究都是建立在测量原始岩体温度的基础上。
All experimental investigations about the geothermal conditions are based on measurements of original rock temperatures.
大陆科学钻探温度测量，为今后进一步研究超高压变质带深部地热场及其地球动力学含义提供了可靠的基础数据。
Temperature measurements and its long-period observation will provide reliable basic data for geothermal and geodynamical study of the ultra-high pressure metamorphic belt.
热储温度是地热研究和地热资源开发中一个重要参数，但直接测量深部热储温度有时有困难。
Geothermal reservoir temperature is one of important parameters in geothermal research and in development of geothermal resources.
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