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物探与化探  2025, Vol. 49 Issue (5): 1030-1038    DOI: 10.11720/wtyht.2025.0036
  地质调查资源勘查 本期目录 | 过刊浏览 | 高级检索 |
张北地区天然氢气藏远景区分析评价——基于重力和大地电磁测深的基底构造解释
万燕鸣1(), 刘玲2,3(), 宿鑫1, 梁帅4, 高雪峰2
1.国能氢创科技(北京)有限责任公司,北京 100007
2.北京天成元能源有限公司,北京 100070
3.应急管理部国家自然灾害防治研究院,北京 100085
4.河北省地质矿产勘查开发局 第三地质大队,河北 张家口 075000
Prospect area analysis and evaluation of natural hydrogen reservoirs in the Zhangbei area: Interpretation of basement structures based on gravity and magnetotelluric sounding
WAN Yan-Ming1(), LIU Ling2,3(), SU Xin1, LIANG Shuai4, GAO Xue-Feng2
1. CEIC Hydrogen Innovation Technology (Beijing) Co., Ltd., Beijing 100007, China
2. Beijing Tianchengyuan Energy Co., Ltd., Beijing 100070, China
3. National Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, China
4. No. 3 Geological Party, Hebei Bureau of Geology and Mineral Resources Exploration, Zhangjiakou 075000, China
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摘要 

在张北盆地的土壤氢气地球化学调查中发现了大面积氢气逸出异常,急需通过地球物理方法了解盆地内具有生氢和导氢作用的基底构造特征。为此,首次在张北盆地开展了针对天然氢的重力和大地电磁调查,在研究区内部署了1∶5万重力和大地电磁测量,基于采集的重力和大地电磁数据,以钻井、地质、物性等资料作为约束,反演了一条横跨研究区的大比例尺重力—大地电磁剖面,确定了盆地“两凹三隆”的构造格局,计算得到中新生代盆地总的沉积厚度为0.62~1.9 km;揭示了4条隐伏断裂,其中F1及F4断裂可作为天然氢运移和存储通道;反演结果显示的两个凹陷内地层界面连续稳定、砂岩—泥岩组合层较厚,可有效减少氢气的泄漏,具有良好的封存能力。本次基底构造研究成果可作为区内天然氢远景区评价以及下一步勘查工作部署的重要基础,同时为建立天然氢勘查技术体系和优选勘探靶区提供了重要依据。

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万燕鸣
刘玲
宿鑫
梁帅
高雪峰
关键词 天然氢重力勘查大地电磁勘查重力-大地电磁约束反演张北地区基底构造    
Abstract

Large-area hydrogen escape anomalies were detected during the soil hydrogen geochemical survey in the Zhangbei Basin, making it urgent to apply geophysical methods to understand the basement structures that generate and transport hydrogen. For this purpose, the first gravity and magnetotelluric surveys targeting natural hydrogen were conducted in the Zhangbei Basin, with 1∶50,000 gravity and magnetotelluric surveys performed within the study area. Using the collected gravity and magnetotelluric data, a large-scale gravity-magnetotelluric profile across the study area was inverted, constrained by drilling, geological, and physical property data. The study identified a "two depressions and three uplifts" structural pattern in the basin, with a total Mesozoic-Cenozoic sedimentary thickness ranging from 0.62 to 1.9 km. Four concealed faults were revealed, among which faults F1 and F4 can serve as migration pathways and storage channels for natural hydrogen. The inversion results indicate that the two depressions exhibited continuous and stable stratigraphic interfaces and relatively thick sandstone-mudstone assemblage layers, which provide good sealing capacity to reduce hydrogen leakage effectively. These findings on basement structures offer valuable insights for the prospect area evaluation of natural hydrogen and subsequent exploration plans in the area. They also provide a significant basis for establishing a natural hydrogen exploration technology system and selecting optimal exploration targets.

Key wordsnatural hydrogen    gravity exploration    magnetotelluric sounding    joint inversion of gravity and magnetotelluric data with constraints    Zhangbei area    basement structure
收稿日期: 2025-02-17      修回日期: 2025-07-04      出版日期: 2025-10-20
ZTFLH:  P631  
基金资助:国能氢创科技(北京)有限责任公司项目“中国天然氢勘察关键技术研究”
通讯作者: 刘玲(1986-),女,博士,高级工程师,主要从事地球物理勘查及天然氢研究工作。Email:liuling860718@163.com
作者简介: 万燕鸣(1985-),男,博士,高级工程师,研究方向为能源经济、氢能。Email:wanyanming@chnenergy.com.cn
引用本文:   
万燕鸣, 刘玲, 宿鑫, 梁帅, 高雪峰. 张北地区天然氢气藏远景区分析评价——基于重力和大地电磁测深的基底构造解释[J]. 物探与化探, 2025, 49(5): 1030-1038.
WAN Yan-Ming, LIU Ling, SU Xin, LIANG Shuai, GAO Xue-Feng. Prospect area analysis and evaluation of natural hydrogen reservoirs in the Zhangbei area: Interpretation of basement structures based on gravity and magnetotelluric sounding. Geophysical and Geochemical Exploration, 2025, 49(5): 1030-1038.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2025.0036      或      https://www.wutanyuhuatan.com/CN/Y2025/V49/I5/1030
Fig.1  张北盆地地质构造略图(根据文献[19]修改)
Ⅰ—华北地块西部;Ⅱ—华北地块中央造山带;Ⅲ—华北地块东部;Ⅳ—秦岭-大别山造山带
Fig.2  研究区布格重力异常分布、大地电磁测线以及沿线氢气浓度分布
Fig.3  不同构造单元典型视电阻率曲线
地层性 密度/(103 kg·m-3) 电阻率 密度层平均密度 电性层
变化范围 平均值 (Ω·m) (103 kg·m-3)
新生界 Q 1.42~1.88 1.68 10~65 1.68
N2s 1.75~1.86 1.81 8~100 2.02 中低
N1h 1.95~2.49 2.22 34~2046
中生界 K 1.80~2.83 2.47 - 2.47 中等
J 1.97~3.13 2.47 86~267
元古宇 PT 2.12~3.75 2.71 - 2.71 -
太古宇 AR 2.26~3.50 2.71 200~2000
Table 1  张北盆地及邻区物性统计
Fig.4  重力—大地电磁联合反演综合地质解释成果
钻孔编号 新生界 中生界 太古宇
第四系 新近系 白垩系
ZK11 - 117.5 257.7 -
ZK15 - 94.6 - -
ZK0828 2.55 34.9 1031.86 >1038.17
ZK0412 6.75 104.41 959.83 >1073
Table 2  钻孔地层埋深
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