The formation, distribution and fault structure of underground thermal water has a close relationship with the Mesozoic granitic magmatic activity.
地下热水的形成和分布与断裂构造及中生代花岗质岩浆活动具有密切关系。
Its characteristics about fault development, fault distribution and fault compound structure are correlate with meridional fault existed early and show a sectional activity.
它的发育、展布、组合结构等特征都与先存的南北向断裂紧密相关，并表现出明显的分段活动特性。
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