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物探与化探  2022, Vol. 46 Issue (6): 1419-1424    DOI: 10.11720/wtyht.2022.1514
  地质调查·资源勘查 本期目录 | 过刊浏览 | 高级检索 |
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1(), 任康辉2, 姜鑫1, 丁保艳1, 童品贤1, 胡沛青2()
1.甘肃省地质矿产勘查开发局 第三地质矿产勘查院,甘肃 兰州 730050
2.兰州大学 地质科学与矿产资源学院,甘肃 兰州 730000
Application of the activated charcoal radon measurement in the geothermal exploration:A study of the Zhangye-Minle basin
LIANG Yu-Dong1(), REN Kang-Hui2, JIANG Xin1, DING Bao-Yan1, TONG Pin-Xian1, HU Pei-Qing2()
1. The Third Institute of Geology and Minerals Exploration, Gansu Provincial Bureau of Geology and Minerals Exploration and Development, Lanzhou 730050, China
2. School of Earth Sciences, Lanzhou University, Lanzhou 730000, China
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摘要 

地热的运移和聚集主要沿断裂带进行,查明勘查区的断裂构造是地热勘探的重要目标。张掖—民乐盆地内断裂众多,且埋藏深,地表难以发现,特殊的地质条件使得传统物探方法的优势无法得到有效发挥。活性炭测氡法抗干扰性强、探测深度大、成本低,在探测隐伏构造方面具有独特优势。本次勘查在张掖—民乐盆地应用活性炭测氡法进行隐伏构造研究,通过对氡浓度测量值的趋势分析,提取局部异常,确定了研究区地下热水勘查有利部位,并为进一步进行钻探和浅层人工地震勘探创造了条件。

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梁雨东
任康辉
姜鑫
丁保艳
童品贤
胡沛青
关键词 活性炭测氡法隐伏断裂地热勘查张掖—民乐盆地    
Abstract

Geothermal energy mainly migrates and accumulates along fractured zones. Ascertaining the faults in the study area is an important goal of geothermal exploration. Many faults are distributed in the Zhangye-Minle basin. They are deeply buried and are difficult to find on the surface. The special geological conditions make it difficult to fully utilize the advantages of conventional geophysical methods. By contrast, the activated charcoal radon measurement features strong anti-interference, large detection depth, and low cost, which are unique advantages in detecting concealed structures. This study investigated the concealed structures in the Zhangye-Minle basin using the activated charcoal radon measurement. Through the trend analysis of measured radon concentrations, this study extracted local anomalies and determined the favorable parts for the geothermal water exploration in the study area, creating conditions for further drilling and shallow artificial seismic exploration.

Key wordsactive carbon method for radon measurement    concealed fault    geothermal exploration    Zhangye-Minle basin
收稿日期: 2021-09-09      修回日期: 2022-06-24      出版日期: 2022-12-20
ZTFLH:  TE132  
基金资助:甘肃省地质勘查基金项目(201602-D28)
通讯作者: 胡沛青
作者简介: 梁雨东(1972-),男,水工环高级工程师,研究方向水文地质、工程地质、地热勘查。Email:273263558@qq.com
引用本文:   
梁雨东, 任康辉, 姜鑫, 丁保艳, 童品贤, 胡沛青. 活性炭测氡法在地热勘探中的应用——以张掖—民乐盆地为例[J]. 物探与化探, 2022, 46(6): 1419-1424.
LIANG Yu-Dong, REN Kang-Hui, JIANG Xin, DING Bao-Yan, TONG Pin-Xian, HU Pei-Qing. Application of the activated charcoal radon measurement in the geothermal exploration:A study of the Zhangye-Minle basin. Geophysical and Geochemical Exploration, 2022, 46(6): 1419-1424.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2022.1514      或      https://www.wutanyuhuatan.com/CN/Y2022/V46/I6/1419
Fig.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.2  张掖—民乐盆地活性炭吸附测氡法平面布置
1—地热井ZK1;2—测线;3—试验线;4—六坝正断层
Fig.3  活性炭吸附测氡法氡值剖面
Fig.4  研究区地表氡气异常平面
1—地热井ZK1;2—六坝正断层;3—推测断层;4—氡值等值线;5—测线;6—推测地热源钻孔
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