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银川盆地东缘上地壳电性结构特征及地热勘探方向

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随着银川盆地东缘地热井的成功实施,指明了围绕黄河断裂及其次级断裂寻找地热的新方向.为了进一步研究黄河断裂对银川盆地东缘地热资源的控制作用及缩小勘探靶区,共布设了 4 条 MT 测线,获得了 71 个测深点.通过对大地电磁测深资料进行预处理及二维反演,获得了研究区 10 km以浅的二维电性结构.综合研究区以往地质、重力、微动、可控源音频大地电磁测深资料,对银川盆地东缘地层、断裂构造进一步解释,认为大地电磁测深测线所反映的奥陶系基底高阻内出现的相对低阻可能是黄河断裂后缘次级断裂发育部位,由奥陶系破碎充水所致,具有地热资源勘探的潜力.
Electrical structure characteristics and geothermal exploration directions of the upper crust on the eastern margin of the Yinchuan Basin
The successful operation of geothermal wells on the eastern margin of the Yinchuan Basin suggests a new geothermal explora-tion orientation around the Huanghe fault and its secondary faults.To further investigate the controlling effect of the Huanghe fault on geothermal resources in the study area and pinpoint the exploration target,this study arranged four magnetotelluric(MT)lines,obtai-ning 71 survey points.The preprocessing and two-dimensional inversion of MT data yielded a two-dimensional electrical structure of the study area within a depth of 10 km.Based on the previous geological,gravity,microtremor,and controllable source audio magnetotellu-rics(CSAMT)data in the study area,this study further interpreted the strata and fault structures of the study area.It posited that the relatively-low-resistivity zone within the high-resistivity zone of the Ordovician basement reflected by the MT lines may be the seconda-ry-fault development site at the rear edge of the Huanghe fault,which is caused by the fragmentation and water filling of Ordovician strata,showing certain exploration potential for geothermal resources.

eastern margin of the Yinchuan Basinelectrical structuregeothermal exploration

仵阳、赵福元、虎新军、陈晓晶、卜进兵、郭少鹏

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宁夏回族自治区地球物理地球化学调查院(自治区深地探测中心),宁夏 银川 750001

中国地质大学(武汉)资源学院,湖北 武汉 430074

银川盆地东缘 电性结构 地热勘探

宁夏自然科学基金项目宁夏自然科学基金项目2022年度宁夏回族自治区财政项目宁夏深部探测方法研究示范创新团队项目

2022AAC036512023AAC05066NXCZ20220206KJT2019005

2024

物探与化探
中国国土资源航空物探遥感中心

物探与化探

CSTPCD
影响因子:0.828
ISSN:1000-8918
年,卷(期):2024.48(5)
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