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南温泉位于重庆东南约30公里的花溪河畔。热水出露于南温泉背斜的两翼,东翼有南温泉热水,西翼有小泉热水;南部近背斜倾没端有桥口坝热水揭露。据实地调查,南温泉地区主要出露嘉陵江组地层,其灰岩溶蚀洼地、溶洞、地下暗河等岩溶景观相当发育。地下热水储集于嘉陵江组第二段角砾状灰岩(T_1j~2)中,水型为SO_4—Ca、Mg型,矿
South Hot Springs is located about 30 km southeast of Chongqing Huaxi River. Hot water is exposed in the wings of the south hot spring anticline. There are hot springs in the south and the Koizumi hot water in the east, and Qiaokou dam hot water in the south near the anticline. According to the field investigation, the South Hot Spring area mainly exposes the Jialingjiang Formation strata, and the limestone dissolution depressions, karst caves and underground underground rivers are quite developed. Underground hot water is stored in the second segment of Jialingjiang breccia limestone (T_1j ~ 2), the water type is SO_4-Ca, Mg type, ore