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遥感和地质构造研究及水文调查表明 ,桂林市西部地区地热主要和断裂有关 ,泉水点多沿断裂展布 ,成热主要受龙胜 -永福断裂带控制 ,该断裂带是主要的导、储热构造 ,两江 -渡头复向斜中的次级褶皱及层间破碎带也是重要的储热构造 ,热储类型以断裂破碎型为主 ,龙胜 -永福断裂带张性断裂活动明显的地段以及和NE ,NW ,EW向断裂交汇地段是最有利的成热部位。
Remote sensing and geological structure studies and hydrological surveys show that the geothermal in the western part of Guilin City is mainly related to faults and the springs are mostly distributed along the faults. The heat generation is mainly controlled by the Longsheng-Yongfu fault zone, which is the main guide for heat storage The secondary folds and interlayer crustal zones in the Liangjiang-Toudou synclinorium are also important thermal storage structures. The main types of thermal reservoirs are fractured and crushed, and the sections of Longsheng-Yongfu fault zone with obvious tensile activity and NE, NW, EW to the intersection of the fault zone is the most favorable heat into the site.