Analysis of the geological genesis of the physical therapy thermal mineral water in the middle section of the western flank of the Lizhi Beach anticline
Lizhi Beach physiotherapy hot mineral water wells are excavated in the middle of the west wing of Lizhi Beach backslope,located in Group 14,Changhe Village,Tongtan Town,Jiangyang District,Luzhou City,Sichuan Province,and contain iron,bromine and metaborate physiotherapy hot mineral water. To investigate the genesis of the Lizhi Beach physiotherapy Thermal Mineral Water by analyzing the geological structure,water source,heat source,thermal storage parameters and hydro-geochemical characteristics of the thermal mineral water. The results are predictable:There are four types of shallow groundwater types in the Lizhi Beach anticline. loose stacked layer pore diving,clastic rock-like pore fissure water,red layer interlayer pressurized water and carbonate rock-like fissure cavern water. Litchi Beach physical therapy hot mineral water is located in the middle of the western wing of the Lizhi Beach anticline,its geological structure and stratigraphic outcrop characteristics are continuous,conducive to receiving atmospheric precipitation replenishment,hot mineral water mineralisation mechanism is mainly for the groundwater through the deep cycle of receiving the geothermal temperature field to form hot water normal warming of the deep circulation of the hydrothermal runoff buried "hot mineral water mineralisation model,the development of paleokarsts The development of ancient karst provides a favourable channel and storage space for the transport and storage of groundwater,and eventually forms iron,bromine and boron therapeutic hot mineral water. The conclusions of the study provide geological information for the development of physiotherapeutic thermal mineral water resources in the region,as well as for the genesis patterns of other hot springs on the region.
thermal mineral wateranalysis of causesdeep cycleTongtan Town
万方数据
维普
