活性炭测氡法在地热勘探中的应用——以张掖—民乐盆地为例

梁雨东, 任康辉, 姜鑫, 丁保艳, 童品贤, 胡沛青

Application of the activated charcoal radon measurement in the geothermal exploration:A study of the Zhangye-Minle basin

LIANG Yu-Dong, REN Kang-Hui, JIANG Xin, DING Bao-Yan, TONG Pin-Xian, HU Pei-Qing

图1 张掖—民乐盆地区域构造(a)及剖面图(b) 1—中下更新统;2—上更新统;3—全新统;4—新近系;5—古近系;6—二叠系;7—石炭系;8—震旦系;9—花岗岩;10—实测断层;11—隐伏断层;12—钻孔ZK1

Fig.1 Regional structure(a) and profile (b) of Zhangye-Minle basin 1—middle and lower Pleistocene; 2—upper Pleistocene; 3—Holocene; 4—Neogene; 5—Paleogene; 6—Permian; 7—Carboniferous; 8—Sinian; 9—granite; 10—measured faults; 11—concealed fault; 12—drill hole ZK1