摘要
山东省天然温泉有18处，自70年代至今，又相继发现地下热水出露点20处。地下热水的赋存形式为层状和带、脉状，其中基岩山区及沂沐断裂带的热储多为带、脉状；鲁西、鲁北平原区的热储多为微倾斜的连续层状或不连续层状，且具多层叠加特征。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。
There are 18 natural thermal springs in Shandong. Accompanying with wild development of the geological exploration job, 20 more spots have been found. The occurrence form of underground thermal water are layer, band and belt types. In the basement mountainous areas and. the Yishu fault,the forms are belt and band types,while in the western and northern plate of Shandong,they are continous and uncontinous layers and has the characteristic of stacked layers. The formation,distribution and fault structure of underground thermal water has a close relationship with the Mesozoic granitic magmatic activity.
出处
《山东地质》
1997年第2期48-53,共6页
Geology of Shandong
