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赣南花岗岩区深部地热岩体电性结构特征研究

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赣南地区地热资源丰富,但对地热资源的开发与利用程度较低,主要是缺乏对地壳深部地热地质体结构特征的研究.本次研究在前人研究基础上,通过大地电磁等地球物理工作对研究区深部结构特征进行研究,建立地热成因机制.以赣南花岗岩地质体为研究对象,使用宽频大地电磁探测法,利用大地电磁测深多测点-多频点阻抗张量成像技术,通过共轭阻抗法分解出电性主轴统计玫瑰图、测点分布云图进行大地线性构造识别,并使用精细二维反演技术推测地质结构特征,对地热异常体进行成像,开展宁都县小布镇地下热水运移机理研究并提供地热钻孔井位.得出结论为,研究区随测点、频点变化的区域电性主轴方位呈线性规律分布,因此存在较为明显的线性构造,且大地构造二维性强,适宜二维反演;确定了目标靶区的热水运移机理为高热流与高产热花岗岩体的多级次断裂控热导水,确定了两条主要控热控水断裂F6、F7;在控热控水断裂处提供900 m钻孔靶位,经打井论证,成功打出热水.
Research on the Electrical Structural Characteristics of Deep Geothermal Rock Mass in Granite Area of Southern Jiangxi
Southern Jiangxi Province is rich in geothermal resources,but the lack of research on the deep geothermal geological structure characteristics restricts the development and re-search of regional geothermal resources.On the basis of previous studies,this paper studied the deep structural characteristics through magnetotelluric method and other geophysical work,and established the geothermal genesis mechanism.Taking the granite geological body in southern Jiangxi as the research object,this paper decomposed the statistical rose di-agram of geo-electrical strike,frequency-based cloud maps,site-based cloud image and struc-tural dimension parameters by using magnetotelluric multi-site,multi-frequency tensor de-composition,and then used fine two-dimensional inversion technology to infer the geological structure characteristics and image the geothermal anomalies.Finally,the mechanism of un-derground hot water migration in Xiaobu Town of Ningdu County was studied to identify the geothermal borehole location.The paper concludes that in the study area,the azimuth of the regional electrical spindle varies with the measurement points and frequency points,and a relatively obvious linear structure is identified with the strong geotectonic two-dimensional structure,which is suitable for two-dimensional inversion.The mechanism of hot water mi-gration in the target area is determined to be multi-stage faults of high heat flow and high yield hot granite rock mass,and two main faults F6 and F7 are identified.A 900m drilling target is provided at the hot-water control fracture,and the hot water is successfully pro-duced after well drilling.

granitebroadband magnetotelluric methodimpedance tensor imagingmigra-tion of hot water

王维强、孙双振

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中国地质科学院水文地质环境地质研究所,河北石家庄 050061

自然资源部地热与干热岩勘查开发技术创新中心,河北石家庄 050061

河北省地质矿产勘查开发局第五地质大队,河北唐山 063000

花岗岩 宽频大地电磁法 阻抗张量成像 热水运移

中国地质调查局地质调查项目

DD20230539

2024

工程地球物理学报
中国地质大学(武汉),长江大学

工程地球物理学报

CSTPCD
影响因子:0.994
ISSN:1672-7940
年,卷(期):2024.21(4)
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