Paleogeotherm field is the key factor for sandstone diagenesis.
古地温场是决定砂岩成岩作用的关键因素。
Paleogeotherm indicates high thermal flow of the upper mantle below the Tan Lu fault zone.
古地温线特征表明,断裂带之下的上地幔具有高的大地热流值。
Paleogeotherm is important for understanding the thermal structure of lithosphere at a specific geological time.
古地温曲线是岩石圈在特定地质时期热结构的集中体现。
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