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青海省水文地质人员在共和地区经过详细工作发现一个埋藏不深的热水自流盆地。含水地层的时代属早更新世及晚第三纪,形成一个向斜构造。热水水温一般在40℃以上。钻孔内热水的
Qinghai hydrogeologists in the Republic after detailed work found a buried hot water basin. Aquifer strata of the era are Early Pleistocene and late Tertiary, forming a syncline structure. Hot water temperature generally above 40 ℃. Drilling holes in the hot water