The Iow-mineralized alkaline silicic thermal waters are distributed mainly in moder intense crustal movement regions and have a direct bearing on the tectinic movements of region fault, depression and foredeep erc.

• 低矿化碱性硅质热水多分布在挽近地壳运动强烈区,与区域构造断裂、断陷、拗陷边缘等构造活动有关。