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古地温曲线是岩石圈在特定地质时期热结构的集中体现。采用矿物地质温压计是建立古地温曲线的基本途径。对比研究发现，适于建立古地温曲线的温压计有Ｂｒｅｙ和Ｋｏｈｌｅｒ（１９９０）、Ｂｅｒｔｒａｎｄ和Ｍｅｒｃｉｅｒ（１９８５）的二辉石温度计，Ｅｌｉｓ和Ｇｒｅｅｎ（１９７９）、Ｋｒｏｇｈ（１９８８）、Ｂｅｒｍａｎ等（１９９５）的石榴石单斜辉石Ｆｅ２＋—Ｍｇ交换反应温度计，Ｎｉｃｋｅｌ和Ｇｒｅｅｎ（１９８５）、Ｂｒｅｙ和Ｋｏｈｌｅｒ（１９９０）的石榴石斜方辉石Ａｌ压力计，以及Ｐｕｔｒｉｋａ等（１９９６）的单斜辉石玄武质熔体平衡温压计
The paleotemperature curve is a concentrated manifestation of the thermal structure of the lithosphere during a specific geological period. The use of mineral geothermometer is to establish the ancient geotemperature curve of the basic way. Comparative studies have found that thermometers suitable for the establishment of paleotemperature profiles include the diatomite thermometers of Brey and Kohler (1990), Bertrand and Mercier (1985), Elis and Green (1979), Krogh (1988), Berman et al. (1995) ) Garnet clinopyroxene Fe2 + -Mg exchange reaction thermometer, Nickel and Green (1985), a garnet orthoclase Al pressure gauge by Brey and Kohler (1990), and the clinopyroxene of Putrika et al. (1996) Basaltic melt balance thermometer