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聊城市城区西部临清拗陷区地下热水在水平方向上的水文地球化学特征具有明显的块段性,大致可分为F2断裂以东和F2断裂以西两个块段,这两个块段地下热水在主要离子组分、微量元素和特征系数等方面均有一定差异。本文根据地下热水水化学资料,判断出了F2断裂的大致位置,同时从地下热水水化学特征的块段性差异和地下热水的变质程度两个方面说明了F2断裂的判断依据。
The hydrogeochemical characteristics of the underground hot water in the horizontal section of the Linqing depression in the west of Liaocheng City have obvious block characteristics and can be roughly divided into two blocks east of the F2 fault and the west of the F2 fault. The two blocks Underground hot water in the main ion composition, trace elements and the coefficient of characteristics are some differences. In this paper, the general location of F2 fracture is judged according to the hydrate chemistry data of underground hot water. At the same time, the judgment basis of F2 fracture is illustrated from the block difference of hydrochemical characteristics of underground hot water and the degree of metamorphism of underground hot water.